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2. Dynamics of recent landslides (

Author

Guimpier, A., Conway, S.J., Mangeney, A., Lucas, A., Mangold, N., Peruzzetto, M., Pajola, M., Lucchetti, A., Munaretto, G., Sæmundsson, T., Johnsson, A., Le Deit, L., Grindrod, P., Davis, J., Thomas, N., and Cremonese, G.

Published
2021
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5. The SuperCam Instrument Suite on the Mars 2020 Rover: Science Objectives and Mast-Unit Description

Author

Maurice, S., Wiens, R. C., Bernardi, P., Caïs, P., Robinson, S., Nelson, T., Gasnault, O., Reess, J.-M., Deleuze, M., Rull, F., Manrique, J.-A., Abbaki, S., Anderson, R. B., André, Y., Angel, S. M., Arana, G., Battault, T., Beck, P., Benzerara, K., Bernard, S., Berthias, J.-P., Beyssac, O., Bonafous, M., Bousquet, B., Boutillier, M., Cadu, A., Castro, K., Chapron, F., Chide, B., Clark, K., Clavé, E., Clegg, S., Cloutis, E., Collin, C., Cordoba, E. C., Cousin, A., Dameury, J.-C., D’Anna, W., Daydou, Y., Debus, A., Deflores, L., Dehouck, E., Delapp, D., De Los Santos, G., Donny, C., Doressoundiram, A., Dromart, G., Dubois, B., Dufour, A., Dupieux, M., Egan, M., Ervin, J., Fabre, C., Fau, A., Fischer, W., Forni, O., Fouchet, T., Frydenvang, J., Gauffre, S., Gauthier, M., Gharakanian, V., Gilard, O., Gontijo, I., Gonzalez, R., Granena, D., Grotzinger, J., Hassen-Khodja, R., Heim, M., Hello, Y., Hervet, G., Humeau, O., Jacob, X., Jacquinod, S., Johnson, J. R., Kouach, D., Lacombe, G., Lanza, N., Lapauw, L., Laserna, J., Lasue, J., Le Deit, L., Le Mouélic, S., Le Comte, E., Lee, Q.-M., Legett, IV, C., Leveille, R., Lewin, E., Leyrat, C., Lopez-Reyes, G., Lorenz, R., Lucero, B., Madariaga, J. M., Madsen, S., Madsen, M., Mangold, N., Manni, F., Mariscal, J.-F., Martinez-Frias, J., Mathieu, K., Mathon, R., McCabe, K. P., McConnochie, T., McLennan, S. M., Mekki, J., Melikechi, N., Meslin, P.-Y., Micheau, Y., Michel, Y., Michel, J. M., Mimoun, D., Misra, A., Montagnac, G., Montaron, C., Montmessin, F., Moros, J., Mousset, V., Morizet, Y., Murdoch, N., Newell, R. T., Newsom, H., Nguyen Tuong, N., Ollila, A. M., Orttner, G., Oudda, L., Pares, L., Parisot, J., Parot, Y., Pérez, R., Pheav, D., Picot, L., Pilleri, P., Pilorget, C., Pinet, P., Pont, G., Poulet, F., Quantin-Nataf, C., Quertier, B., Rambaud, D., Rapin, W., Romano, P., Roucayrol, L., Royer, C., Ruellan, M., Sandoval, B. F., Sautter, V., Schoppers, M. J., Schröder, S., Seran, H.-C., Sharma, S. K., Sobron, P., Sodki, M., Sournac, A., Sridhar, V., Standarovsky, D., Storms, S., Striebig, N., Tatat, M., Toplis, M., Torre-Fdez, I., Toulemont, N., Velasco, C., Veneranda, M., Venhaus, D., Virmontois, C., Viso, M., Willis, P., and Wong, K. W.

Published
2021
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8. Multi-Mission GIS for the ExoMars Rover Mission’s Oxia Planum Landing Site

Author

Sefton-Nash, E., Fawdon, P., Orgel, C., Balme, M., Quantin-Nataf, C., torres, I., Volat, M., Hauber, Ernst, Adeli, Solmaz, Davis, J., Grindrod, P.M., Frigeri, A., Le Deit, L., Loizeau, Damien, Nass, A., Ruesch, O., Taylor, C., de Witte, S., Vago, J., and The ExoMars, 'Macro' group

Subjects
online GIS, Mapping, Oxia Planum, MMGIS, Geology, ExoMars
Published
2022

11. Fluorine and Lithium at the Kimberley Outcrop, Gale Crater

Author

Forni, O, Vaniman, D. T, Le Deit, L, Clegg, S. M, Lanza, N. L, Lasue, J, Bish, D. L, Mangold, N, Wiens, R. C, Meslin, P.-Y, Gasnault, O, Maurice, S, Cousin, A, Toplis, M. J, Newsom, H, and Rampe, E. B

Subjects
Lunar And Planetary Science And Exploration
Abstract

ChemCam is an active remote sensing instrument which has operated successfully on MSL since landing in August, 2012. Its laser pulses remove dust and to profile through weathering coatings of rocks up to 7 m away. Laser-induced breakdown spectroscopy (LIBS) produces emission spectra of materials ablated from the samples in electronically excited states. As the plasma cools, elements can recombine and molecular emission lines are observed. Recent experiments have shown that some of these molecular emissions can be much brighter than the associated atomic lines, especially when halo-gens and rare earth elements are present. We observed these molecular emissions in some of the ChemCam spectra and report the first detection of chlorine and fluorine with ChemCam. It is also the first time ever that fluorine has been detected on the surface of Mars. Among all the F-bearing observations, one third are observed in the Kimberley outcrop. We will dis-cuss the potential mineralogies related to these observations as well as the related elemental correlations and propose interpretations.

Published
2015

12. The SuperCam Instrument Suite on the Mars 2020 Rover: Science Objectives and Mast-Unit Description

Author

Química analítica, Kimika analitikoa, Maurice, Sylvestre, Wiens, Roger C., Bernardi, Pernelle, Cais, Philippe, Robinson, Scott H., Nelson, T., Gasnault, Olivier, Reess, Jean-Michel, Deleuze, Muriel, Rull, Fernando, Manrique, José Antonio, Abbaki, S., Anderson, Ryan B., Andre, Yves, Angel, S. M., Arana Momoitio, Gorka, Battault, T., Beck, Pierre, Benzerara, Karim, Bernard, Sylvain, Berthias, J. P., Beyssac, Olivier, Bonafous, M., Bousquet, Bruno, Boutillier, M., Cadu, A., Castro Ortiz de Pinedo, Kepa, Chapron, F., Chide, Baptiste, Clark, Kevin, Clavé, E., Clegg, Sam, Cloutis, Edward, Collin, C., Cordoba, Elizabeth C., Cousin, Agnes, Dameury, J. C., D'Anna, W., Daydou, Y., Debus, A., Deflores, Lauren, Dehouck, E., Delapp, Dorothea, De Los Santos, G., Donny, Christophe, Doressoundiram, A., Dromart, Gilles, Dubois, Bruno, Dufour, A., Dupieux, M., Egan, Miles, Ervin, Joan, Fabre, Cecile, Fau, Amaury, Fischer, Woodward, Forni, Olivie, Fouchet, Thierry, Frydenvang, Jens, Gauffre, S., Gauthier, M., Gharakanian, V., Gilard, O., Gontijo, Ivair, González, R., Granena, D., Grotzinger, John, Hassen Khodja, R., Heim, M., Hello, Y., Hervet, G., Humeau, O., Jacob, Xavier, Jacquinod, Sophie, Johnson, Jeffrey R., Kouach, D., Lacombe, G., Lanza, Nina, Lapauw, L., Laserna, Javier, Lasue, Jeremie, Le Deit, L., Le Comte, E., Lee, Q. M., Legett, Carey, Leveille, Richard, Lewin, Eric, Leyrat, C., López Reyes, Guillermo, Lorenz, Ralph, Lucero, Briana, Madariaga, J. M., Madsen, Soren, Madsen, Morten, Mangold, Nicolas, Manni, F., Mariscal, J. F., Martínez Frías, Jesús, Mathieu, K., Mathon, R., McCabe, Kevin P., McConnochie, Timothy H., McLennan, Scott M., Mekki, J., Melikechi, Noureddine, Meslin, Pierre-Yves, Micheau, Y., Michel, Y., Michel, John M., Mimoun, David, Misra, Anupam, Montagnac, Gilles, Montaron, C., Montmessin, Franck, Moros, J., Mousset, Valerie, Morizet, Y., Murdoch, Naomi, Newell, Raymond T., Newsom, Horton, Tuong, N. N., Ollila, Ann M., Orttner, G., Oudda, L., Pares, Laurent, Parisot, J., Parot, Yann, Pérez, R., Pheav, D., Picot, L., Pilleri, Paolo, Pilorget, C., Pinet, Patrick, Pont, Gabriel, Poulet, Francois, Quantin-Nataf, C., Quertier, Benjamin, Rambaud, D., Rapin, William, Romano, Philip J., Roucayrol, L., Royer, Clement, Ruellan, M., Sandoval, Benigno, Sautter, Violaine, Schoppers, Marcel J., Schroder, S., Seran, H. C., Sharma, Shiv K., Sobrón, Pablo, Sodki, M., Sournac, A., Sridhar, Vishnu, Standarovsky, D., Storms, Steven, Striebig, N., Tatat, M., Toplis, Michael J., Torre Fernández, Imanol, Toulemont, N., Velasco, C., Veneranda, Marco, Venhaus, Dawn, Virmontois, C., Viso, M., Willis, Peter, Wong, K. W., Química analítica, Kimika analitikoa, Maurice, Sylvestre, Wiens, Roger C., Bernardi, Pernelle, Cais, Philippe, Robinson, Scott H., Nelson, T., Gasnault, Olivier, Reess, Jean-Michel, Deleuze, Muriel, Rull, Fernando, Manrique, José Antonio, Abbaki, S., Anderson, Ryan B., Andre, Yves, Angel, S. M., Arana Momoitio, Gorka, Battault, T., Beck, Pierre, Benzerara, Karim, Bernard, Sylvain, Berthias, J. P., Beyssac, Olivier, Bonafous, M., Bousquet, Bruno, Boutillier, M., Cadu, A., Castro Ortiz de Pinedo, Kepa, Chapron, F., Chide, Baptiste, Clark, Kevin, Clavé, E., Clegg, Sam, Cloutis, Edward, Collin, C., Cordoba, Elizabeth C., Cousin, Agnes, Dameury, J. C., D'Anna, W., Daydou, Y., Debus, A., Deflores, Lauren, Dehouck, E., Delapp, Dorothea, De Los Santos, G., Donny, Christophe, Doressoundiram, A., Dromart, Gilles, Dubois, Bruno, Dufour, A., Dupieux, M., Egan, Miles, Ervin, Joan, Fabre, Cecile, Fau, Amaury, Fischer, Woodward, Forni, Olivie, Fouchet, Thierry, Frydenvang, Jens, Gauffre, S., Gauthier, M., Gharakanian, V., Gilard, O., Gontijo, Ivair, González, R., Granena, D., Grotzinger, John, Hassen Khodja, R., Heim, M., Hello, Y., Hervet, G., Humeau, O., Jacob, Xavier, Jacquinod, Sophie, Johnson, Jeffrey R., Kouach, D., Lacombe, G., Lanza, Nina, Lapauw, L., Laserna, Javier, Lasue, Jeremie, Le Deit, L., Le Comte, E., Lee, Q. M., Legett, Carey, Leveille, Richard, Lewin, Eric, Leyrat, C., López Reyes, Guillermo, Lorenz, Ralph, Lucero, Briana, Madariaga, J. M., Madsen, Soren, Madsen, Morten, Mangold, Nicolas, Manni, F., Mariscal, J. F., Martínez Frías, Jesús, Mathieu, K., Mathon, R., McCabe, Kevin P., McConnochie, Timothy H., McLennan, Scott M., Mekki, J., Melikechi, Noureddine, Meslin, Pierre-Yves, Micheau, Y., Michel, Y., Michel, John M., Mimoun, David, Misra, Anupam, Montagnac, Gilles, Montaron, C., Montmessin, Franck, Moros, J., Mousset, Valerie, Morizet, Y., Murdoch, Naomi, Newell, Raymond T., Newsom, Horton, Tuong, N. N., Ollila, Ann M., Orttner, G., Oudda, L., Pares, Laurent, Parisot, J., Parot, Yann, Pérez, R., Pheav, D., Picot, L., Pilleri, Paolo, Pilorget, C., Pinet, Patrick, Pont, Gabriel, Poulet, Francois, Quantin-Nataf, C., Quertier, Benjamin, Rambaud, D., Rapin, William, Romano, Philip J., Roucayrol, L., Royer, Clement, Ruellan, M., Sandoval, Benigno, Sautter, Violaine, Schoppers, Marcel J., Schroder, S., Seran, H. C., Sharma, Shiv K., Sobrón, Pablo, Sodki, M., Sournac, A., Sridhar, Vishnu, Standarovsky, D., Storms, Steven, Striebig, N., Tatat, M., Toplis, Michael J., Torre Fernández, Imanol, Toulemont, N., Velasco, C., Veneranda, Marco, Venhaus, Dawn, Virmontois, C., Viso, M., Willis, Peter, and Wong, K. W.

Abstract

On the NASA 2020 rover mission to Jezero crater, the remote determination of the texture, mineralogy and chemistry of rocks is essential to quickly and thoroughly characterize an area and to optimize the selection of samples for return to Earth. As part of the Perseverance payload, SuperCam is a suite of five techniques that provide critical and complementary observations via Laser-Induced Breakdown Spectroscopy (LIBS), Time-Resolved Raman and Luminescence (TRR/L), visible and near-infrared spectroscopy (VISIR), high-resolution color imaging (RMI), and acoustic recording (MIC). SuperCam operates at remote distances, primarily 2-7 m, while providing data at sub-mm to mm scales. We report on SuperCam's science objectives in the context of the Mars 2020 mission goals and ways the different techniques can address these questions. The instrument is made up of three separate subsystems: the Mast Unit is designed and built in France; the Body Unit is provided by the United States; the calibration target holder is contributed by Spain, and the targets themselves by the entire science team. This publication focuses on the design, development, and tests of the Mast Unit; companion papers describe the other units. The goal of this work is to provide an understanding of the technical choices made, the constraints that were imposed, and ultimately the validated performance of the flight model as it leaves Earth, and it will serve as the foundation for Mars operations and future processing of the data.

Published
2021

13. The SuperCam Instrument Suite on the Mars 2020 Rover:Science Objectives and Mast-Unit Description

Author

Maurice, S., Wiens, R. C., Bernardi, P., Caïs, P., Robinson, S., Nelson, T., Gasnault, O., Reess, J. M., Deleuze, M., Rull, F., Manrique, J. A., Abbaki, S., Anderson, R. B., André, Y., Angel, S. M., Arana, G., Battault, T., Beck, P., Benzerara, K., Bernard, S., Berthias, J. P., Beyssac, O., Bonafous, M., Bousquet, B., Boutillier, M., Cadu, A., Castro, K., Chapron, F., Chide, B., Clark, K., Clavé, E., Clegg, S., Cloutis, E., Collin, C., Cordoba, E. C., Cousin, A., Dameury, J. C., D’Anna, W., Daydou, Y., Debus, A., Deflores, L., Dehouck, E., Delapp, D., De Los Santos, G., Donny, C., Doressoundiram, A., Dromart, G., Dubois, B., Dufour, A., Dupieux, M., Egan, M., Ervin, J., Fabre, C., Fau, A., Fischer, W., Forni, O., Fouchet, T., Frydenvang, J., Gauffre, S., Gauthier, M., Gharakanian, V., Gilard, O., Gontijo, I., Gonzalez, R., Granena, D., Grotzinger, J., Hassen-Khodja, R., Heim, M., Hello, Y., Hervet, G., Humeau, O., Jacob, X., Jacquinod, S., Johnson, J. R., Kouach, D., Lacombe, G., Lanza, N., Lapauw, L., Laserna, J., Lasue, J., Le Deit, L., Le Mouélic, S., Le Comte, E., Lee, Q. M., Legett, C., Leveille, R., Lewin, E., Leyrat, C., Lopez-Reyes, G., Lorenz, R., Lucero, B., Madariaga, J. M., Madsen, S., Madsen, M., Mangold, N., Manni, F., Mariscal, J. F., Martinez-Frias, J., Mathieu, K., Mathon, R., McCabe, K. P., McConnochie, T., McLennan, S. M., Mekki, J., Melikechi, N., Meslin, P.-Y., Micheau, Y., Michel, Y., Michel, J. M., Mimoun, D., Misra, A., Montagnac, G., Montaron, C., Montmessin, F., Moros, J., Mousset, V., Morizet, Y., Murdoch, N., Newell, R. T., Newsom, H., Nguyen Tuong, N., Ollila, A. M., Orttner, G., Oudda, L., Pares, L., Parisot, J., Parot, Y., Pérez, R., Pheav, D., Picot, L., Pilleri, P., Pilorget, C., Pinet, P., Pont, G., Poulet, F., Quantin-Nataf, C., Quertier, B., Rambaud, D., Rapin, W., Romano, P., Roucayrol, L., Royer, C., Ruellan, M., Sandoval, B. F., Sautter, V., Schoppers, M. J., Schröder, S., Seran, H. C., Sharma, S. K., Sobron, P., Sodki, M., Sournac, A., Sridhar, V., Standarovsky, D., Storms, S., Striebig, N., Tatat, M., Toplis, M., Torre-Fdez, I., Toulemont, N., Velasco, C., Veneranda, M., Venhaus, D., Virmontois, C., Viso, M., Willis, P., Wong, K. W., Maurice, S., Wiens, R. C., Bernardi, P., Caïs, P., Robinson, S., Nelson, T., Gasnault, O., Reess, J. M., Deleuze, M., Rull, F., Manrique, J. A., Abbaki, S., Anderson, R. B., André, Y., Angel, S. M., Arana, G., Battault, T., Beck, P., Benzerara, K., Bernard, S., Berthias, J. P., Beyssac, O., Bonafous, M., Bousquet, B., Boutillier, M., Cadu, A., Castro, K., Chapron, F., Chide, B., Clark, K., Clavé, E., Clegg, S., Cloutis, E., Collin, C., Cordoba, E. C., Cousin, A., Dameury, J. C., D’Anna, W., Daydou, Y., Debus, A., Deflores, L., Dehouck, E., Delapp, D., De Los Santos, G., Donny, C., Doressoundiram, A., Dromart, G., Dubois, B., Dufour, A., Dupieux, M., Egan, M., Ervin, J., Fabre, C., Fau, A., Fischer, W., Forni, O., Fouchet, T., Frydenvang, J., Gauffre, S., Gauthier, M., Gharakanian, V., Gilard, O., Gontijo, I., Gonzalez, R., Granena, D., Grotzinger, J., Hassen-Khodja, R., Heim, M., Hello, Y., Hervet, G., Humeau, O., Jacob, X., Jacquinod, S., Johnson, J. R., Kouach, D., Lacombe, G., Lanza, N., Lapauw, L., Laserna, J., Lasue, J., Le Deit, L., Le Mouélic, S., Le Comte, E., Lee, Q. M., Legett, C., Leveille, R., Lewin, E., Leyrat, C., Lopez-Reyes, G., Lorenz, R., Lucero, B., Madariaga, J. M., Madsen, S., Madsen, M., Mangold, N., Manni, F., Mariscal, J. F., Martinez-Frias, J., Mathieu, K., Mathon, R., McCabe, K. P., McConnochie, T., McLennan, S. M., Mekki, J., Melikechi, N., Meslin, P.-Y., Micheau, Y., Michel, Y., Michel, J. M., Mimoun, D., Misra, A., Montagnac, G., Montaron, C., Montmessin, F., Moros, J., Mousset, V., Morizet, Y., Murdoch, N., Newell, R. T., Newsom, H., Nguyen Tuong, N., Ollila, A. M., Orttner, G., Oudda, L., Pares, L., Parisot, J., Parot, Y., Pérez, R., Pheav, D., Picot, L., Pilleri, P., Pilorget, C., Pinet, P., Pont, G., Poulet, F., Quantin-Nataf, C., Quertier, B., Rambaud, D., Rapin, W., Romano, P., Roucayrol, L., Royer, C., Ruellan, M., Sandoval, B. F., Sautter, V., Schoppers, M. J., Schröder, S., Seran, H. C., Sharma, S. K., Sobron, P., Sodki, M., Sournac, A., Sridhar, V., Standarovsky, D., Storms, S., Striebig, N., Tatat, M., Toplis, M., Torre-Fdez, I., Toulemont, N., Velasco, C., Veneranda, M., Venhaus, D., Virmontois, C., Viso, M., Willis, P., and Wong, K. W.

Abstract

On the NASA 2020 rover mission to Jezero crater, the remote determination of the texture, mineralogy and chemistry of rocks is essential to quickly and thoroughly characterize an area and to optimize the selection of samples for return to Earth. As part of the Perseverance payload, SuperCam is a suite of five techniques that provide critical and complementary observations via Laser-Induced Breakdown Spectroscopy (LIBS), Time-Resolved Raman and Luminescence (TRR/L), visible and near-infrared spectroscopy (VISIR), high-resolution color imaging (RMI), and acoustic recording (MIC). SuperCam operates at remote distances, primarily 2–7 m, while providing data at sub-mm to mm scales. We report on SuperCam’s science objectives in the context of the Mars 2020 mission goals and ways the different techniques can address these questions. The instrument is made up of three separate subsystems: the Mast Unit is designed and built in France; the Body Unit is provided by the United States; the calibration target holder is contributed by Spain, and the targets themselves by the entire science team. This publication focuses on the design, development, and tests of the Mast Unit; companion papers describe the other units. The goal of this work is to provide an understanding of the technical choices made, the constraints that were imposed, and ultimately the validated performance of the flight model as it leaves Earth, and it will serve as the foundation for Mars operations and future processing of the data.

Published
2021

15. Martian polar and circum-polar sulfate-bearing deposits: Sublimation tills derived from the North Polar Cap

Author

Masse, M., Bourgeois, O., Le Mouelic, S., Verpoorter, C., Le Deit, L., and Bibring, J.P.

Subjects
Chlorates -- Analysis, Sand dunes -- Analysis, Sediments (Geology) -- Analysis, Gypsum -- Analysis, Glaciers -- Analysis, Ice caps -- Analysis, Astronomy, Earth sciences
Abstract

To link to full-text access for this article, visit this link: http://dx.doi.org/10.1016/j.icarus.2010.04.017 Byline: M. Masse (a), O. Bourgeois (a), S. Le Mouelic (a), C. Verpoorter (a)(b), L. Le Deit (a)(c), J.P. Bibring (d) Keywords: Mars, Polar caps; Mars, Polar geology; Mineralogy; Ices, IR spectroscopy; Mars, Surface Abstract: Previous spectroscopic studies have shown the presence of hydrated minerals in various kinds of sedimentary accumulations covering and encircling the martian North Polar Cap. More specifically, gypsum, a hydrated calcium sulfate, has been detected on Olympia Planum, a restricted part of the Circum-Polar Dune Field. To further constrain the geographical distribution and the process of formation and accumulation of these hydrated minerals, we performed an integrated morphological, structural and compositional analysis of a key area where hydrated minerals were detected and where the main polar landforms are present. By the development of a spectral processing method based on spectral derivation and by the acquisition of laboratory spectra of gypsum-ice mixtures we find that gypsum-bearing sediment is not restricted to the Olympia Planum dunes but is also present in all kinds of superficial sediment covering the surface of the North Polar Cap and the Circum-Polar Dune Field. Spectral signatures consistent with perchlorates are also detected on these deposits. The interpretation of landforms reveals that this gypsum-bearing sediment was released from the ice cap by sublimation. We thus infer that gypsum crystals that are now present in the Circum-Polar Dune Field derive from the interior of the North Polar Cap. Gypsum crystals that were initially trapped in the ice cap have been released by sublimation of the ice and have accumulated in the form of ablation tills at the surface of the ice cap. These gypsum-bearing sublimation tills are reworked by winds and are transported towards the Circum-Polar Dune Field. Comparison with sulfates found in terrestrial glaciers suggests that gypsum crystals in the martian North Polar Cap have formed by weathering of dust particles, either in the atmosphere prior to their deposition during the formation of the ice cap, and/or in the ice cap after their deposition. Author Affiliation: (a) Laboratoire de Planetologie et Geodynamique, UMR 6112, CNRS, Universite de Nantes, 2 chemin de la Houssiniere, BP 92205, 44322 Nantes Cedex 3, France (b) Laboratoire d'Oceanologie et de Geosciences, UMR LOG 8187, 32 Avenue Foch, 62930 Wimereux, France (c) Institute of Planetary Research, German Aerospace Center (DLR), Rutherfordstr. 2, 12489 Berlin, Germany (d) Institut d'Astrophysique Spatiale, Universite' Paris XI, Orsay, France Article History: Received 22 January 2010; Revised 21 April 2010; Accepted 21 April 2010

Published
2010

16. Morphology, stratigraphy, and mineralogical composition of a layered formation covering the plateaus around Valles Marineris, Mars: Implications for its geological history

Author

Le Deit, L., Bourgeois, O., Mege, D., Hauber, E., Le Mouelic, S., Masse, M., Jaumann, R., and Bibring, J.-P.

Subjects
Mars (Planet) -- Analysis, Astronomy -- Analysis, Geomorphology -- Analysis, Astronomy, Earth sciences
Abstract

To link to full-text access for this article, visit this link: http://dx.doi.org/10.1016/j.icarus.2010.03.012 Byline: L. Le Deit (a)(b), O. Bourgeois (b), D. Mege (b), E. Hauber (a), S. Le Mouelic (b), M. Masse (b), R. Jaumann (a), J.-P. Bibring (c) Keywords: Geological processes; Mars, Surface; Mineralogy Abstract: An extensive layered formation covers the high plateaus around Valles Marineris. Mapping based on HiRISE, CTX and HRSC images reveals these layered deposits (LDs) crop out north of Tithonium Chasma, south of Ius Chasma, around West Candor Chasma, and southwest of Juventae Chasma and Ganges Chasma. The estimated area covered by LDs is [approximately equal to]42,300km.sup.2. They consist of a series of alternating light and dark beds, a 100m in total thickness that is covered by a dark unconsolidated mantle possibly resulting from their erosion. Their stratigraphic relationships with the plateaus and the Valles Marineris chasmata indicate that the LDs were deposited during the Early- to Late Hesperian, and possibly later depending on the region, before the end of the backwasting of the walls near Juventae Chasma, and probably before Louros Valles sapping near Ius Chasma. Their large spatial coverage and their location mainly on highly elevated plateaus lead us to conclude that LDs correspond to airfall dust and/or volcanic ash. The surface of LDs is characterized by various morphological features, including lobate ejecta and pedestal craters, polygonal fractures, valleys and sinuous ridges, and a pitted surface, which are all consistent with liquid water and/or water ice filling the pores of LDs. LDs were episodically eroded by fluvial processes and were possibly modified by sublimation processes. Considering that LDs correspond to dust and/or ash possibly mixed with ice particles in the past, LDs may be compared to Dissected Mantle Terrains currently observed in mid- to high latitudes on Mars, which correspond to a mantle of mixed dust and ice that is partially or totally dissected by sublimation. The analysis of CRISM and OMEGA hyperspectral data indicates that the basal layer of LDs near Ganges Chasma exhibits spectra with absorption bands at [approximately equal to]1.4[mu]m, and [approximately equal to]1.9[mu]m and a large deep band between [approximately equal to]2.21 and [approximately equal to]2.26[mu]m that are consistent with previous spectral analysis in other regions of LDs. We interpret these spectral characteristics as an enrichment of LDs in opaline silica or by Al-phyllosilicate-rich layers being overlain by hydroxylated ferric sulfate-rich layers. These alteration minerals are consistent with the aqueous alteration of LDs at low temperatures. Author Affiliation: (a) Institute of Planetary Research, German Aerospace Center (DLR), Berlin, Germany (b) Laboratoire de Planetologie et de Geodynamique de Nantes, CNRS UMR-6112, Universite de Nantes, France (c) Institut d'Astrophysique Spatiale, Universite Paris 11, Orsay Campus, France Article History: Received 14 October 2009; Revised 3 March 2010; Accepted 10 March 2010

Published
2010

17. Characterization of small sedimentary structures in rocks of the Glen Torridon region (Gale crater, Mars) using photogrammetry

Author

Gwénaël CARAVACA, Nicolas Mangold, Stéphane Le Mouélic, Le Deit, L., Gasnault, O., Rivera-Hernandez, F., Fedo, C., Edgett, K., Wiens, R., Laboratoire de Planétologie et Géodynamique [UMR 6112] (LPG), Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST), Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Institut de recherche en astrophysique et planétologie (IRAP), Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), Darmouth College [Hanover, New Hampshire], Department of Earth and Planetary Sciences [Knoxville], The University of Tennessee [Knoxville], Malin Space Science Systems (MSSS), Los Alamos National Laboratory (LANL), Lunar & Planetary Institute, European Project: 776276,PLANMAP, Institut national des sciences de l'Univers (INSU - CNRS)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP), and Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)

Subjects
Sedimentary structures, [SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology, Stratigraphy, Photogrammetry, [SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy, Mars, [SDU.STU]Sciences of the Universe [physics]/Earth Sciences, Glen Torridon, Digital Outcrop Model, Gale crater, Sedimentology
Abstract

International audience; The Glen Torridon (GT) region in Gale crater, Mars, has been explored by the Mars Science Laboratory Curiosity rover since ~Sol 2300 (Feb. '19), seeking traces of the clay-bearing minerals initially detected from orbiter data [1]. The lowermost locations of the GT trough are dominated by the Jura member mudstones, and fine-grained sandstones of the Knockfarril Hill member above it. The latter exhibit multi-scale laminations and cross-bedding. The precise characterization of these sedimentary structures is critical for understanding the stratigraphic relationships between the GT members, but also the hydrodynamical conditions that prevailed during deposition of these sediments. Some of the smallest structures encountered by Curiosity were observed using the Mars Hand Lens Im-ager (MAHLI) instrument which can resolve coarse silt (62.5 μm) at a distances of ~2 to 4 cm. In this study, we use MAHLI images and Structure-from-Motion (SfM) photogrammetry to reconstruct 3D micro Digital Out-crop Models (DOM) of GT rocks for interpreting small-scale 3D sedimentary structures.

Published
2020

18. Estimating kaolinite crystallinity using near-infrared spectroscopy

Author

Pineau, M., Baron, F., Mathian, M., Le Deit, L., Rondeau, B., Allard, T., Mangold, N., Laboratoire de Planétologie et Géodynamique UMR6112 (LPG), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Nantes - Faculté des Sciences et des Techniques, Université de Nantes (UN)-Université de Nantes (UN)-Université d'Angers (UA), Institut de Chimie des Milieux et Matériaux de Poitiers (IC2MP), Université de Poitiers-Centre National de la Recherche Scientifique (CNRS), Institut de minéralogie, de physique des matériaux et de cosmochimie (IMPMC), Muséum national d'Histoire naturelle (MNHN)-Institut de recherche pour le développement [IRD] : UR206-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Planétologie et Géodynamique [UMR 6112] (LPG), Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST), Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), and Université de Poitiers-Institut national des sciences de l'Univers (INSU - CNRS)-Institut de Chimie du CNRS (INC)-Centre National de la Recherche Scientifique (CNRS)

Subjects
[CHIM.CRIS]Chemical Sciences/Cristallography, ComputingMilieux_MISCELLANEOUS, [SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
Abstract

International audience

Published
2020

19. Deposition and erosion of a Light-Toned Yardang-forming unit of Mt Sharp, Gale crater, Mars

Author

Dromart, G., primary, Le Deit, L., additional, Rapin, W., additional, Gasnault, O., additional, Le Mouélic, S., additional, Quantin-Nataf, C., additional, Mangold, N., additional, Rubin, D., additional, Lasue, J., additional, Maurice, S., additional, Newsom, H.E., additional, Pinet, P., additional, Scuderi, L., additional, and Wiens, R.C., additional

Published
2021
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20. Geological significance of hydrated silica on Mars as seen by CRISM data compared to terrestrial analogs

Author

Pineau, M., Le Deit, L., Chauviré, B., Carter, J., Rondeau, B., Mangold, N., Laboratoire de Planétologie et Géodynamique UMR6112 (LPG), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Nantes - Faculté des Sciences et des Techniques, Université de Nantes (UN)-Université de Nantes (UN)-Université d'Angers (UA), Institut des Sciences de la Terre (ISTerre), Université Grenoble Alpes (UGA)-Centre National de la Recherche Scientifique (CNRS)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-PRES Université de Grenoble-Institut de recherche pour le développement [IRD] : UR219-Institut national des sciences de l'Univers (INSU - CNRS)-Institut Français des Sciences et Technologies des Transports, de l'Aménagement et des Réseaux (IFSTTAR)-Université Joseph Fourier - Grenoble 1 (UJF), Institut d'astrophysique spatiale (IAS), Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Planétologie et Géodynamique [UMR 6112] (LPG), Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST), Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Institut Français des Sciences et Technologies des Transports, de l'Aménagement et des Réseaux (IFSTTAR)-Institut national des sciences de l'Univers (INSU - CNRS)-Institut de recherche pour le développement [IRD] : UR219-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes [2016-2019] (UGA [2016-2019]), Pineau, Maxime, and Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Centre National d’Études Spatiales [Paris] (CNES)

Subjects
[SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology, [SDU.STU.PL] Sciences of the Universe [physics]/Earth Sciences/Planetology, ComputingMilieux_MISCELLANEOUS, [SDU.STU.MI] Sciences of the Universe [physics]/Earth Sciences/Mineralogy, [SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
Abstract

International audience

Published
2019

21. Classification of 59 Igneous Rocks Analyzed by ChemCam at Gale Crater, Mars

Author

Cousin, A., Sautter, V., Payré, V., Forni, O., Mangold, N., Gasnault, O., Le Deit, L., Meslin, P. Y., Johnson, J., Maurice, S., Wiens, R. C., William Rapin, Laboratoire de Planétologie et Géodynamique [UMR 6112] (LPG), Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST), Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Institut de recherche en astrophysique et planétologie (IRAP), Institut national des sciences de l'Univers (INSU - CNRS)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP), Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS), and Los Alamos National Laboratory (LANL)

Subjects
[SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology
Abstract

International audience; Chemistry, mineralogy, texture, and petrology of the 59 igneous rocks analyzed by ChemCam (MSL), and comparison with igneous rocks observed by the Mars Exploration Rovers as well as with the Mars meteorites.

Published
2019

22. Fluorine on Mars: Seven Years of Detection with ChemCam On-Board MSL

Author

Forni, O., Meslin, P.-Y., Cousin, A., Mangold, N., Le Deit, L., Gasnault, O., David, G., Nachon, M., Blaney, D., Newson, H., Maurice, S., Wiens, R. C., Gaft, M., Institut de recherche en astrophysique et planétologie (IRAP), Institut national des sciences de l'Univers (INSU - CNRS)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP), Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS), DLR Institute of Planetary Research, German Aerospace Center (DLR), Laboratoire de Planétologie et Géodynamique [UMR 6112] (LPG), Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST), Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Jet Propulsion Laboratory (JPL), NASA-California Institute of Technology (CALTECH), and Los Alamos National Laboratory (LANL)

Subjects
[SDU.ASTR.EP]Sciences of the Universe [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP], [SDU.STU]Sciences of the Universe [physics]/Earth Sciences, [PHYS.ASTR]Physics [physics]/Astrophysics [astro-ph]
Abstract

International audience; We report fluorine detection by ChemCam on board MSL-curiosity during its traverse. We present the geological settings in which it is found and propose some interpretaion about the mineralogical phases it is found and their respective formation.

Published
2019

23. Correction of Stray Light in CHEMCAM Remote Micro-Imager Long Distance Images

Author

Stéphane Le Mouélic, Gasnault, O., Herkenhoff, K. E., Newsom, H. E., Gallegos, Z., William Rapin, Anderson, R. B., Le Deit, L., Mangold, N., Dromart, G., Johnson, J. R., Maurice, S., Wiens, R. C., Laboratoire de Planétologie et Géodynamique [UMR 6112] (LPG), Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST), Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Institut de recherche en astrophysique et planétologie (IRAP), Institut national des sciences de l'Univers (INSU - CNRS)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP), Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS), Institute of Meteoritics [Albuquerque] (IOM), The University of New Mexico [Albuquerque], Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement [Lyon] (LGL-TPE), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-École normale supérieure - Lyon (ENS Lyon), Los Alamos National Laboratory (LANL), Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement (LGL-TPE), École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL), and Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS)

Subjects
Computer Science::Robotics, [SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology, Computer Science::Computer Vision and Pattern Recognition, Astrophysics::Instrumentation and Methods for Astrophysics, Astrophysics::Cosmology and Extragalactic Astrophysics, Astrophysics::Galaxy Astrophysics
Abstract

International audience; We discuss the radiometric correction of a bright halo that is observed in some long distance images taken by the ChemCam/RMI camera onboard Curiosity.

Published
2019

25. Chemical alteration of fine-grained sedimentary rocks at Gale crater

Author

Mangold, Nicolas, Dehouck, E., Fedo, C., Forni, Olivier, Achilles, C., Bristow, T., Downs, R. T., Frydenvang, J., Gasnault, Olivier, L'Haridon, J., Le Deit, L., Maurice, Sylvestre, McLennan, S. M., Meslin, Pierre-Yves, Morrison, S., Newsom, H. E., Rampe, E., Rapin, William, Rivera-Hernandez, F., Salvatore, M., Mangold, Nicolas, Dehouck, E., Fedo, C., Forni, Olivier, Achilles, C., Bristow, T., Downs, R. T., Frydenvang, J., Gasnault, Olivier, L'Haridon, J., Le Deit, L., Maurice, Sylvestre, McLennan, S. M., Meslin, Pierre-Yves, Morrison, S., Newsom, H. E., Rampe, E., Rapin, William, Rivera-Hernandez, F., and Salvatore, M.

Abstract

From Sol 750 to 1550, the Curiosity rover documented>100 m thick stack of fine-grained sedimentary rocks making up part of the Murray formation, at the base of Mt Sharp, Gale crater. Here, we use data collected by the ChemCam instrument to estimate the level of chemical weathering in these sedimentary rocks. Both the Chemical Index of Alteration (CIA) and the Weathering Index Scale (WIS) indicate a progressive increase in alteration up section, reaching values of CIA of 63 and WIS of 25%. The increase in CIA and WIS values is coupled with a decrease in calcium abundance, suggesting partial dissolution of Ca-bearing minerals (clinopyroxene and plagioclase). Mineralogy from the CheMin X-ray diffraction instrument indicates a decrease in mafic minerals compared with previously analyzed strata and a significant proportion of phyllosilicates consistent with this interpretation. These observations suggest that the sediments were predominantly altered in an open system, before or during their emplacement, contrasting with the rock-dominated conditions inferred in sedimentary deposits analyzed at Yellowknife Bay.

Published
2019

26. Reconstructing paleoenvironments in Robert Sharp Crater, Mars: Evidence for a fluvio-lacustrine system

Author

Brossier, Jérémy F., Le Deit, L., Hauber, Ernst, Mangold, N., Carter, J., and Jaumann, R.

Subjects
Planetengeologie, Robert Sharp crater, Geological mapping, Mars geology
Abstract

Recent mineralogical studies suggest the presence of an iron chlorine hydroxide, namely akaganeite. This mineral is known to form under specific conditions, and it has been detected in the Robert Sharp Crater, located at Mars’ low-latitudes (133.59˚E, -4.12˚N) [1]. Its detection implies an acidic and oxidizing environment in this region. Indeed, akaganeite typically forms in highly saline and chlorinated aqueous environments on Earth. These akaganeite deposits might be the ultimate alteration phase of a drying lake within the Robert Sharp Crater. Hence, we carried out morphological and stratigraphical studies, as well as age determination by crater counting to constrain the geological and hydrological history of the region [2]. We found that the Robert Sharp Crater has known a varied geological history, including the formation of fretted terrains and an airfall filling during the Hesperian epoch. Furthermore, the presence of valleys and fan-shaped deposits, and the detection of various aqueous minerals, in the region suggest the possibility of a fluvio-lacustrine activity phase within the crater during the last period of the Martian chronology, also named Amazonian epoch. The presence of a putative paleolake should be short-time and estimated between 1.3 Ga and 500 Ma. Thus, by reconstructing the paleoenvironments in the Robert Sharp Crater, we demonstrate that Mars has known several episodes of aqueous activities well after the late Noachian/ early Hesperian period. References: [1] Carter, J. et al. (2015) Icarus, 253. [2] Brossier, J. F. et al. (in prep).

Published
2018

27. Investigation of opals on MARS using CRISM data and terrestrial analogs

Author

Pineau, M., Le Deit, L., Rondeau, B., Chauviré, B., Carter, J., Mangold, N., Laboratoire de Planétologie et Géodynamique [UMR 6112] (LPG), Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST), Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Institut des Sciences de la Terre (ISTerre), Institut Français des Sciences et Technologies des Transports, de l'Aménagement et des Réseaux (IFSTTAR)-Institut national des sciences de l'Univers (INSU - CNRS)-Institut de recherche pour le développement [IRD] : UR219-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes [2016-2019] (UGA [2016-2019]), Institut d'astrophysique spatiale (IAS), Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Centre National d’Études Spatiales [Paris] (CNES), Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Pineau, Maxime, Laboratoire de Planétologie et Géodynamique UMR6112 (LPG), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Nantes - Faculté des Sciences et des Techniques, Université de Nantes (UN)-Université de Nantes (UN)-Université d'Angers (UA), and Université Grenoble Alpes (UGA)-Centre National de la Recherche Scientifique (CNRS)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-PRES Université de Grenoble-Institut de recherche pour le développement [IRD] : UR219-Institut national des sciences de l'Univers (INSU - CNRS)-Institut Français des Sciences et Technologies des Transports, de l'Aménagement et des Réseaux (IFSTTAR)-Université Joseph Fourier - Grenoble 1 (UJF)

Subjects
[SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology, [SDU.STU.PL] Sciences of the Universe [physics]/Earth Sciences/Planetology, ComputingMilieux_MISCELLANEOUS, [SDU.STU.MI] Sciences of the Universe [physics]/Earth Sciences/Mineralogy, [SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
Abstract

International audience

Published
2018

28. Landing Sites for a Mars Sample Return Mission in Arabia Terra

Author

Salese, Francesco, Pondrelli, Monica, Schmidt, G., Mitri, G., Pacifici, A., Cavalazzi, B., Ori, Gian-Gabriele, Glamoclija, Mihaela, Hauber, Ernst, Le Deit, L., Marinangeli, L., and Rossi, A.P.

Subjects
Planetengeologie, geology, life, landing site, water, Mars, sample return
Published
2018

30. Chemical alteration of fine-grained sedimentary rocks at Gale crater

Author

Mangold, N., primary, Dehouck, E., additional, Fedo, C., additional, Forni, O., additional, Achilles, C., additional, Bristow, T., additional, Downs, R.T., additional, Frydenvang, J., additional, Gasnault, O., additional, L'Haridon, J., additional, Le Deit, L., additional, Maurice, S., additional, McLennan, S.M., additional, Meslin, P.-Y., additional, Morrison, S., additional, Newsom, H.E., additional, Rampe, E., additional, Rapin, W., additional, Rivera-Hernandez, F., additional, Salvatore, M., additional, and Wiens, R.C., additional

Published
2019
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31. Alkali trace elements in Gale crater, Mars, with ChemCam: Calibration update and geological implications

Author

Payré, V., Fabre, C., Cousin, A., Sautter, V., Wiens, R., Forni, O., Gasnault, O., Mangold, N., Meslin, P.-Y., Lasue, J., Ollila, A., Rapin, W., Maurice, S., Nachon, M., Le Deit, L., Lanza, N., Clegg, S., Institut de recherche en astrophysique et planétologie (IRAP), Institut national des sciences de l'Univers (INSU - CNRS)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP), Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS), Los Alamos National Laboratory (LANL), Laboratoire de Planétologie et Géodynamique [UMR 6112] (LPG), Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST), Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), and Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS)

Subjects
[SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology, ComputingMilieux_MISCELLANEOUS
Abstract

International audience

Published
2017
Full Text
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32. Deltaic sediments in Magong Crater, Mars

Author

Knade, Julius, Hauber, Ernst, Platz, Thomas, Fanara, Lida, Le Deit, L., and Kinch, K.

Subjects
HRSC, delta, layering, water, Mars, sedimentation, lake
Published
2017

36. The potassic sedimentary rocks in Gale Crater, Mars, as seen by ChemCam on board Curiosity

Author

Le Deit, L, Mangold, N, Forni, O, Cousin, A, Lasue, J, Schroder, S, Wiens, RC, Sumner, D, Fabre, C, Stack, KM, Anderson, RB, Blaney, D, Clegg, S, Dromart, G, Fisk, M, Gasnault, O, Grotzinger, JP, Gupta, S, Lanza, N, Le Mouelic, S, Maurice, S, McLennan, SM, Meslin, P-Y, Nachon, M, Newsom, H, Payre, V, Rapin, W, Rice, M, Sautter, V, Treiman, AH, DLR Institute of Planetary Research, German Aerospace Center (DLR), Laboratoire de Planétologie et Géodynamique [UMR 6112] (LPG), Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST), Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Institut de recherche en astrophysique et planétologie (IRAP), Institut national des sciences de l'Univers (INSU - CNRS)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP), Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS), Los Alamos National Laboratory (LANL), University of California [Davis] (UC Davis), University of California, California Institute of Technology (CALTECH), Jet Propulsion Laboratory (JPL), NASA-California Institute of Technology (CALTECH), Oregon State University (OSU), Department of Physics and Materials Science & Centre for Functional Photonics (CFP), The University of Hong Kong (HKU), Stony Brook University [SUNY] (SBU), State University of New York (SUNY), Laboratoire de Météorologie Dynamique (UMR 8539) (LMD), Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)-École des Ponts ParisTech (ENPC)-École polytechnique (X)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC), Institute of Meteoritics [Albuquerque] (IOM), The University of New Mexico [Albuquerque], Laboratoire Ecologie Fonctionnelle et Environnement (ECOLAB), Institut Ecologie et Environnement (INEE), Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Toulouse III - Paul Sabatier (UT3), Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut National Polytechnique (Toulouse) (Toulouse INP), Université Fédérale Toulouse Midi-Pyrénées, Institut de minéralogie, de physique des matériaux et de cosmochimie (IMPMC), Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut de recherche pour le développement [IRD] : UR206-Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS), Lunar and Planetary Institute [Houston] (LPI), Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), University of California (UC), Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL), Laboratoire Ecologie Fonctionnelle et Environnement (LEFE), Université de Toulouse (UT)-Université de Toulouse (UT)-Observatoire Midi-Pyrénées (OMP), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS)-Institut National Polytechnique (Toulouse) (Toulouse INP), Université de Toulouse (UT), Muséum national d'Histoire naturelle (MNHN)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut de recherche pour le développement [IRD] : UR206-Centre National de la Recherche Scientifique (CNRS), California Institute of Technology (CALTECH)-NASA, Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut Ecologie et Environnement (INEE), Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National Polytechnique (Toulouse) (Toulouse INP), Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP), and Science and Technology Facilities Council (STFC)

Subjects
Geochemistry & Geophysics, SANDSTONE, Science & Technology, INSTRUMENT SUITE, ORIGIN, IN-SITU, ROVER, K-FELDSPAR, EVOLUTION, [SDU]Sciences of the Universe [physics], Physical Sciences, OLIVINE, OUTCROP, SYSTEM, ComputingMilieux_MISCELLANEOUS
Abstract

The Mars Science Laboratory rover Curiosity encountered potassium-rich clastic sedimentary rocks at two sites in Gale Crater, the waypoints Cooperstown and Kimberley. These rocks include several distinct meters thick sedimentary outcrops ranging from fine sandstone to conglomerate, interpreted to record an ancient fluvial or fluvio-deltaic depositional system. From ChemCam Laser-Induced Breakdown Spectroscopy (LIBS) chemical analyses, this suite of sedimentary rocks has an overall mean K2O abundance that is more than 5 times higher than that of the average Martian crust. The combined analysis of ChemCam data with stratigraphic and geographic locations reveals that the mean K2O abundance increases upward through the stratigraphic section. Chemical analyses across each unit can be represented as mixtures of several distinct chemical components, i.e., mineral phases, including K-bearing minerals, mafic silicates, Fe-oxides, and Fe-hydroxide/oxyhydroxides. Possible K-bearing minerals include alkali feldspar (including anorthoclase and sanidine) and K-bearing phyllosilicate such as illite. Mixtures of different source rocks, including a potassium-rich rock located on the rim and walls of Gale Crater, are the likely origin of observed chemical variations within each unit. Physical sorting may have also played a role in the enrichment in K in the Kimberley formation. The occurrence of these potassic sedimentary rocks provides additional evidence for the chemical diversity of the crust exposed at Gale Crater.

Published
2016
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37. The potassic sedimentary rocks in Gale Crater, Mars, as seen by ChemCam on boardCuriosity

Author

Le Deit, L., Mangold, N., Forni, O., Cousin, A., Lasue, J., Schröder, S., Wiens, R. C., Sumner, D., Fabre, C., Stack, K. M., Anderson, R. B., Blaney, D., Clegg, S., Dromart, G., Fisk, M., Gasnault, O., Grotzinger, J. P., Gupta, S., Lanza, N., Le Mouélic, S., Maurice, S., McLennan, S. M., Meslin, P.-Y., Nachon, M., Newsom, H., Payré, V., Rapin, W., Rice, M., Sautter, V., and Treiman, A. H.

Subjects
Mars, Special Section: The Mars Science Laboratory Rover Mission (Curiosity) at The Kimberley, Gale Crater
Published
2016

38. Observation of >5 wt % zinc at the Kimberley outcrop, Gale crater, Mars

Author

Lasue, J., Clegg, S. M., Forni, O., Cousin, A., Wiens, R. C., Lanza, N., Mangold, N., Le Deit, L., Gasnault, O., Maurice, S., Berger, Arjan, Stack, K., Blaney, D., Fabre, Cécile, Goetz, W., Johnson, J., Le Mouélic, S., Nachon, M., Payré, V., Rapin, W., Sumner, D. Y., Institut de recherche en astrophysique et planétologie (IRAP), Institut national des sciences de l'Univers (INSU - CNRS)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP), Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS), Los Alamos National Laboratory (LANL), Laboratoire de Planétologie et Géodynamique [UMR 6112] (LPG), Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST), Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), European Southern Observatory (ESO), California Institute of Technology (CALTECH), Jet Propulsion Laboratory (JPL), NASA-California Institute of Technology (CALTECH), GeoRessources, Institut national des sciences de l'Univers (INSU - CNRS)-Centre de recherches sur la géologie des matières premières minérales et énergétiques (CREGU)-Université de Lorraine (UL)-Centre National de la Recherche Scientifique (CNRS), Johns Hopkins University Applied Physics Laboratory [Laurel, MD] (APL), Laboratoire Ecologie Fonctionnelle et Environnement (ECOLAB), Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut Ecologie et Environnement (INEE), Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National Polytechnique (Toulouse) (Toulouse INP), Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP), Department of Earth and Planetary Science [UC Berkeley] (EPS), University of California [Berkeley], University of California-University of California, Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), Laboratoire Ecologie Fonctionnelle et Environnement (LEFE), Institut Ecologie et Environnement (INEE), Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Observatoire Midi-Pyrénées (OMP), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS)-Institut National Polytechnique (Toulouse) (Toulouse INP), Université de Toulouse (UT), University of California [Berkeley] (UC Berkeley), and University of California (UC)-University of California (UC)

Subjects
data reduction technique, Mars, [SDU.STU]Sciences of the Universe [physics]/Earth Sciences, laser-induced breakdown spectroscopy (LIBS)
Abstract

International audience; Zinc-enriched targets have been detected at the Kimberley formation, Gale crater, Mars, using the Chemistry Camera (ChemCam) instrument. The Zn content is analyzed with a univariate calibration based on the 481.2 nm emission line. The limit of quantification for ZnO is 3 wt % (at 95% confidence level) and 1 wt % (at 68% confidence level). The limit of detection is shown to be around 0.5 wt %. As of sol 950, 12 targets on Mars present high ZnO content ranging from 1.0 wt % to 8.4 wt % (Yarrada, sol 628). Those Zn-enriched targets are almost entirely located at the Dillinger member of the Kimberley formation, where high Mn and alkali contents were also detected, probably in different phases. Zn enrichment does not depend on the textures of the rocks (coarse-grained sandstones, pebbly conglomerates, and resistant fins). The lack of sulfur enhancement suggests that Zn is not present in the sphalerite phase. Zn appears somewhat correlated with Na2O and the ChemCam hydration index, suggesting that it could be in an amorphous clay phase (such as sauconite). On Earth, such an enrichment would be consistent with a supergene alteration of a sphalerite gossan cap in a primary siliciclastic bedrock or a possible hypogene nonsulfide zinc deposition where Zn, Fe, Mn would have been transported in a reduced sulfur-poor fluid and precipitated rapidly in the form of oxides.

Published
2016
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39. ChemCam activities and discoveries during the nominal mission of the Mars Science Laboratory in Gale crater, Mars

Author

Thompson, L., Williams, A., Williams, R., Blaney, D., Calef, F., Dietrich, W., Edgett, K., Fisk, M., Gellert, R., Grotzinger, J., Kah, L., McLennan, S., Palucis, M., Siebach, K., Stack, K., Sumner, D., Yingst, A., Maurice, S., Clegg, S., Wiens, R., Gasnault, O., Rapin, W., Forni, O., Cousin, A., Sautter, V., Mangold, N., Le Deit, L., Nachon, M., Anderson, R., Lanza, N., Fabre, C., Payré, V., Lasue, J., Meslin, P.-Y., Léveillé, R., Barraclough, B., Beck, P., Bender, S., Berger, G., Bridges, J., Bridges, N., Dromart, G., Dyar, M., Francis, R., Frydenvang, J., Gondet, B., Ehlmann, B., Herkenhoff, K., Johnson, J., Langevin, Y., Madsen, M., Melikechi, N., Lacour, J.-L., Le Mouélic, Stéphane, Lewin, E., Newsom, H., Ollila, A., Pinet, P., Schröder, S., Sirven, J.-B., Tokar, R., Toplis, M., D'Uston, C., Vaniman, D., Vasavada, A., Jet Propulsion Laboratory (JPL), California Institute of Technology (CALTECH)-NASA, Oregon State University (OSU), Department of Physics [Guelph], University of Guelph, California Institute of Technology (CALTECH), Stony Brook University [SUNY] (SBU), State University of New York (SUNY), Department of Earth and Planetary Science [UC Berkeley] (EPS), University of California [Berkeley], University of California-University of California, Division of Geological and Planetary Sciences [Pasadena], University of California [Davis] (UC Davis), University of California, Planetary Science Institute [Tucson] (PSI), Institut de recherche en astrophysique et planétologie (IRAP), Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP), Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS), Los Alamos National Laboratory (LANL), Institut de minéralogie, de physique des matériaux et de cosmochimie (IMPMC), Institut de recherche pour le développement [IRD] : UR206-Centre National de la Recherche Scientifique (CNRS)-Muséum national d'Histoire naturelle (MNHN)-Université Pierre et Marie Curie - Paris 6 (UPMC), Laboratoire de Planétologie et Géodynamique UMR6112 (LPG), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Nantes - Faculté des Sciences et des Techniques, Université de Nantes (UN)-Université de Nantes (UN)-Université d'Angers (UA), DLR Institute of Planetary Research, German Aerospace Center (DLR), Laboratoire Ecologie Fonctionnelle et Environnement (ECOLAB), Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut National Polytechnique (Toulouse) (Toulouse INP), Université Fédérale Toulouse Midi-Pyrénées, Laboratoire de Météorologie Dynamique (UMR 8539) (LMD), Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS Paris)-École normale supérieure - Paris (ENS Paris), Canadian Space Agency (CSA), Institut de Planétologie et d'Astrophysique de Grenoble (IPAG), Centre National d'Études Spatiales [Toulouse] (CNES)-Université Grenoble Alpes (UGA)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Grenoble (OSUG), Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Joseph Fourier - Grenoble 1 (UJF)-Centre National de la Recherche Scientifique (CNRS), Space Research Centre [Leicester], University of Leicester, Institut d'astrophysique spatiale (IAS), Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Astrogeology Science Center [Flagstaff], United States Geological Survey [Reston] (USGS), Centre for Infection and Immunity, Optical Science Center for Applied Research (OSCAR), Delaware State University (DSU), Service d'études analytiques et de réactivité des surfaces (SEARS), Département de Physico-Chimie (DPC), CEA-Direction de l'Energie Nucléaire (CEA-DEN), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris-Saclay-CEA-Direction de l'Energie Nucléaire (CEA-DEN), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris-Saclay, Institut des Sciences de la Terre (ISTerre), Université Grenoble Alpes (UGA)-Centre National de la Recherche Scientifique (CNRS)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-PRES Université de Grenoble-Institut de recherche pour le développement [IRD] : UR219-Institut national des sciences de l'Univers (INSU - CNRS)-Institut Français des Sciences et Technologies des Transports, de l'Aménagement et des Réseaux (IFSTTAR)-Université Joseph Fourier - Grenoble 1 (UJF), Institute of Meteoritics [Albuquerque] (IOM), The University of New Mexico [Albuquerque], Technologies et systèmes d'information pour les agrosystèmes (UR TSCF), Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA), Commissariat à l'Energie Atomique et aux Energies Alternatives, Commissariat à l'énergie atomique et aux énergies alternatives (CEA), Dynamique terrestre et planétaire (DTP), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Centre d'étude spatiale des rayonnements (CESR), Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement [Lyon] (LGL-TPE), École normale supérieure - Lyon (ENS Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), NASA-California Institute of Technology (CALTECH), University of California [Berkeley] (UC Berkeley), University of California (UC)-University of California (UC), University of California (UC), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), Muséum national d'Histoire naturelle (MNHN)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut de recherche pour le développement [IRD] : UR206-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Planétologie et Géodynamique [UMR 6112] (LPG), Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST), Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Laboratoire Ecologie Fonctionnelle et Environnement (LEFE), Institut Ecologie et Environnement (INEE), Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Observatoire Midi-Pyrénées (OMP), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS)-Institut National Polytechnique (Toulouse) (Toulouse INP), Université de Toulouse (UT), École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL), Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Observatoire des Sciences de l'Univers de Grenoble (OSUG ), Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes [2016-2019] (UGA [2016-2019])-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes [2016-2019] (UGA [2016-2019]), Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Centre National d’Études Spatiales [Paris] (CNES), CEA-Direction des Energies (ex-Direction de l'Energie Nucléaire) (CEA-DES (ex-DEN)), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris-Saclay-CEA-Direction des Energies (ex-Direction de l'Energie Nucléaire) (CEA-DES (ex-DEN)), Institut Français des Sciences et Technologies des Transports, de l'Aménagement et des Réseaux (IFSTTAR)-Institut national des sciences de l'Univers (INSU - CNRS)-Institut de recherche pour le développement [IRD] : UR219-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes [2016-2019] (UGA [2016-2019]), Institut national des sciences de l'Univers (INSU - CNRS)-Université Toulouse III - Paul Sabatier (UT3), Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS), Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut de recherche pour le développement [IRD] : UR206-Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS), Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut National Polytechnique (Toulouse) (Toulouse INP), Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)-École des Ponts ParisTech (ENPC)-École polytechnique (X)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC), Observatoire Midi-Pyrénées (OMP), and Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Toulouse III - Paul Sabatier (UT3)

Subjects
010504 meteorology & atmospheric sciences, atomic Emission spectroscopy, Mars, Mineralogy, Context (language use), 01 natural sciences, Analytical Chemistry, Atmosphere, laser-spectroscopy, Spectroscopy, ComputingMilieux_MISCELLANEOUS, 0105 earth and related environmental sciences, LIBS, Chemistry, 010401 analytical chemistry, Noachian, Gale crater, Crust, Mars Exploration Program, 15. Life on land, Gale Crater, 0104 chemical sciences, Characterization (materials science), Geochemistry, in-situ, ChemCam, 13. Climate action, [SDU]Sciences of the Universe [physics]
Abstract

At Gale crater, Mars, ChemCam acquired its first laser-induced breakdown spectroscopy (LIBS) target on Sol 13 of the landed portion of the mission (a Sol is a Mars day). Up to Sol 800, more than 188 000 LIBS spectra were acquired on more than 5800 points distributed over about 650 individual targets. We present a comprehensive review of ChemCam scientific accomplishments during that period, together with a focus on the lessons learned from the first use of LIBS in space. For data processing, we describe new tools that had to be developed to account for the uniqueness of Mars data. With regard to chemistry, we present a summary of the composition range measured on Mars for major-element oxides (SiO_2, TiO_2, Al_2O_3, FeO_T, MgO, CaO, Na_2O, K_2O) based on various multivariate models, with associated precisions. ChemCam also observed H, and the non-metallic elements C, O, P, and S, which are usually difficult to quantify with LIBS. F and Cl are observed through their molecular lines. We discuss the most relevant LIBS lines for detection of minor and trace elements (Li, Rb, Sr, Ba, Cr, Mn, Ni, and Zn). These results were obtained thanks to comprehensive ground reference datasets, which are set to mimic the expected mineralogy and chemistry on Mars. With regard to the first use of LIBS in space, we analyze and quantify, often for the first time, each of the advantages of using stand-off LIBS in space: no sample preparation, analysis within its petrological context, dust removal, sub-millimeter scale investigation, multi-point analysis, the ability to carry out statistical surveys and whole-rock analyses, and rapid data acquisition. We conclude with a discussion of ChemCam performance to survey the geochemistry of Mars, and its valuable support of decisions about selecting where and whether to make observations with more time and resource-intensive tools in the rover's instrument suite. In the end, we present a bird's-eye view of the many scientific results: discovery of felsic Noachian crust, first observation of hydrated soil, discovery of manganese-rich coatings and fracture fills indicating strong oxidation potential in Mars' early atmosphere, characterization of soils by grain size, and wide scale mapping of sedimentary strata, conglomerates, and diagenetic materials.

Published
2016
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41. Equatorial Layered Deposits in the Firsoff crater area: process variability and habitability potential

Author

Pondrelli, M., Rossi, A. P., Le Deit, L., Gasselt, S., Fueten, F., Glamoclija, M., BARBARA CAVALAZZI, Hauber, E., Franchi, F., Pondrelli M., Rossi A.P., Le Deit L., van Gasselt S., Fueten F., Glamoclija M., Cavalazzi B., Hauber E., and Franchi F.

Subjects
Mar, Spring deposits, Equatorial Layered Deposit
Abstract

The depositional processes proposed to explain the formation of the Equatorial Layered Deposits (ELDs) on Mars invoke very different systems such as sub-glacial volcanism, aeolian/airfall, lacustrine, lacustrine/volcanic and spring-fed deposition. We performed a detailed geological analysis of Firsoff crater and surrounding areas, where ELDs are present within and outside craters, using all the available datasets. ELDs stay on top of the Noachian Plateau Sequence and are covered by the Hesperian Ridged Plains Material. Within Firsoff crater, ELDs form a central bulge - estimated more than one kilometer thick - while, outside the craters, ELDs form flat-lying deposits probably not thicker than few tens of meters. Inside craters, terraced-like morphologies made of ELDs are found to mark the topographically highest deposits toward the rim. Although locally heavily eroded by wind, ELDs within Firsoff crater and within the other craters of the area show several morphologies that appear to be depositional, which would exclude that the craters were originally filled by ELDs. Within craters, ELDs consist of two facies: a roughly meter thick high albedo layered unit which drape and onlap the Plateau Sequence and hundreds meters large / tens of meters thick cone-shaped mounds made of layered breccia embedded in a matrix. The layered unit is disrupted in a post-depositional polygonal pattern and show no evidence of sedimentary structures. Mounds sometimes display an orifice at the top of their structure. Both facies appear to be linked to and possibly sourced from tectonically controlled fissure ridges. The two facies appear to be stratigraphically in heteropy thus suggesting a temporal as well as a genetic association. Polyhydrated sulfates have been detected in correspondence of ELDs. Outside the craters, ELDs show large-scale cross stratification associated to duneforms. On the base of these morphological, sedimentological and stratigraphic elements, we distinguish between fluid expulsion ELDs forming inside craters and aeolian ELDs outside and the craters. Fluid expulsion ELDs would result from groundwater upwelling and subsequent evaporitic precipitation, whereas aeolian ELDs from reworking and redeposition of the spring ELDs. While the climate supporting such a cycle was likely arid by terrestrial standards, these surface conditions in a terrestrial environment would have been conducive for microbial colonization. The potential for habitable conditions of evaporite settings as shown on analogues on Earth coupled with the high preservation potential within sulfates, make these deposits good candidate to understand the potential past habitability of Mars.

Published
2013

43. Reconstructing the infilling history within Robert Sharp Crater, Mars: Insights from morphology and stratigraphy

Author

Brossier, Jérémy F., Le Deit, L., Hauber, E., Mangold, N., Carter, J., and Jaumann, R.

Subjects
Planetengeologie, remote sensing, morphology, Mars, geological mapping, Robert Sharp
Abstract

According to recent mineralogical study, the presence of an iron oxi-hydroxide (akaganéite) which form under specific conditions, has been detected in Robert Sharp crater, located in the equatorial region of Mars (133.59°'E, -4.12°N), implying an acidic and oxidizing environment in this region. These deposits of akaganéite might be the ultimate alteration phase of a drying lake or lagoon within Robert Sharp. Morphological and stratigraphical studies and, as well, age determination has been carried out in order to constrain the geological and hydrological history of Robert Sharp. Robert Sharp has known a varied geological history, including the formation of fretted terrains and an aerial/aeolian filling during the Hesperian epoch. The presence of valleys and fan-shaped deposits, and the detection of several aqueous minerals, in the crater suggest the presence of a fluvio-lacustrine activity phase in the crater during the last period of the Martian chronology, the Amazonian epoch. The existence of a putative paleo-lake should be short-time and estimated between 1.3 Ga and 500 Ma. Thus, this study shows that Mars has known several phases of aqueous activities well after the late Noachian/ early Hesperian period.

Published
2015

48. Outflow Channels and Associated Fan Deltas: Post-Noachian Fluvial Diversity in the Southern Highlands of Mars

Author

Adeli, Solmaz, Hauber, Ernst, Le Deit, L., Kleinhans, M., Jaumann, Ralf, Geomorfologie, and Coastal dynamics, Fluvial systems and Global change

Subjects
Amazonian, Outflow channel, Mars, Highlands, Fluvial activity
Abstract

A series of outflow channels in the southern highlands of Mars dated as Amazonian, represent evidence for local and limited aqueous environmental conditions and rich post-Noachian aqueous activity.

Published
2014

50. Observation of > 5 wt % zinc at the Kimberley outcrop, Gale crater, Mars

Author

Lasue, J., primary, Clegg, S. M., additional, Forni, O., additional, Cousin, A., additional, Wiens, R. C., additional, Lanza, N., additional, Mangold, N., additional, Le Deit, L., additional, Gasnault, O., additional, Maurice, S., additional, Berger, J. A., additional, Stack, K., additional, Blaney, D., additional, Fabre, C., additional, Goetz, W., additional, Johnson, J., additional, Le Mouélic, S., additional, Nachon, M., additional, Payré, V., additional, Rapin, W., additional, and Sumner, D. Y., additional

Published
2016
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