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393 results on '"Gloaguen, Eric"'

10. Effects of sulfoxide and sulfone sidechain–backbone hydrogen bonding on local conformations in peptide models.

Author

Liu, Dayi, Robin, Sylvie, Gloaguen, Eric, Brenner, Valérie, Mons, Michel, and Aitken, David J.

Subjects
PEPTIDES, HYDROGEN bonding, AMINO acid residues, SULFOXIDES, SYSTEMS design, SPINE, FUNCTIONAL groups
Abstract

We examine peptide model systems designed to probe short-range N–H⋯O＝S sidechain–backbone hydrogen bonding involving amino acid residues with sidechain sulfoxide or sulfone functional groups and its effects on local conformations. A strong 7-membered ring hydrogen bond of this type accompanies an intra-residue N–H⋯O＝C interaction and stabilizes an extended backbone conformation in preference to classical folded structures. [ABSTRACT FROM AUTHOR]

Published
2024
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14. Polyphased rare-element magmatism during late orogenic evolution: geochronological constraints from NW Variscan Iberia

Author

Melleton Jérémie, Gloaguen Eric, Frei Dirk, Lima Alexandre, Vieira Romeu, and Martins Tania

Subjects
rare-element granite and pegmatite, columbite group minerals, la-sf-icpms dating, variscan orogeny, iberian massif, Geology, QE1-996.5
Abstract

Rare-element granites and pegmatites represent important sources of raw materials for “clean, green and high technologies”, such as lithium and tantalum, for example. However, mechanisms of rare-element granites and pegmatite’s origin are still far from being fully understood. Several rare-element pegmatite fields and a rare-element granite are known in the Variscan realms located in Iberia (Spain and Portugal), enhancing the interest of this area for studying the formation of these extremely fractionated melts. In situ U-Pb dating by LA-SF-ICP-MS of columbite-group minerals from rare-element granites and pegmatites of the Iberian Variscan belt provides new constraints on the generation of rare-element melts. Three events have been recognized: (i) Emplacement of the Argemela rare-element granite, in the Central Iberian Zone (CIZ), with an age of 326 ± 3 Ma; (ii) Emplacement of rare-element pegmatites from the Galicia-Trás-os-Montes Zone (GTOMZ), at an average age of 310 ± 5 Ma; (iii) Emplacement of rare-element pegmatites in the CIZ and in the southern GTOMZ at about 301 ± 3 Ma. These two last events are coeval with the two peaks of ages for the late orogenic magmatism at ca. 308 Ma and 299 Ma, and all dated rare-element pegmatites clearly emplaced during the late-orogenic evolution of the Variscan belt. Contemporaneous fields of rare-element pegmatites are arranged in belts following those formed by similar granitoid suites. Pegmatite fields from both the GTOMZ and the CIZ reveal a southward propagation of ages of emplacement, which matches the observed propagation of deformation, metamorphism and magmatism in the two different geotectonic zones. Existence of three successive rare-element events in the Iberian Massif argues against the involvement of lower crustal HP-HT metamorphism in the generation of rare-element melts. Possible sources of rare-element-enriched melts are more likely located in the middle to upper crust, as are the major components of granitic magmatism. Analyses of U and Pb isotopes from columbite-group minerals are very robust and reproducible, making them good candidates for dating ore deposits related to peraluminous magmatism as well as REE- and Nb-bearing deposits.

Published
2022
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16. Isolated Neutral Peptides

Author

Gloaguen, Eric, Mons, Michel, Bayley, Hagan, Series editor, Houk, Kendall N., Series editor, Hughes, Greg, Series editor, Hunter, Christopher A., Series editor, Ishihara, Kazuaki, Series editor, Krische, Michael J, Series editor, Lehn, J.-M., Series editor, Luque, Rafael, Series editor, Olivucci, Massimo, Series editor, Siegel, Jay S., Series editor, Thiem, Joachim, Series editor, Venturi, Margherita, Series editor, Wong, Chi-Huey, Series editor, Wong, Henry N.C., Series editor, You, Shu-Li, Series editor, Rijs, Anouk M., editor, and Oomens, Jos, editor

Published
2015
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18. Genetic relationship between greisenization and Sn–W mineralization in vein and greisen deposits: Insights from the Panasqueira deposit (Portugal)

Author

Launay Gaëtan, Sizaret Stanislas, Lach Philippe, Melleton Jérémie, Gloaguen Eric, and Poujol Marc

Subjects
vein and greisen sn–w deposits, panasqueira, white-mica chemistry, quartz trace chemistry, u–pb dating of apatite, magmatic-hydrothermal evolution, Geology, QE1-996.5
Abstract

The W–Sn Panasqueira ore deposit is a magmatic-hydrothermal system, which includes a high-grade quartz-vein type mineralization and a disseminated greisen-type mineralization occurring in the upper part of the Panasqueira two-mica granite. We investigated the genetic and chronological relationships between the greisenization of the Panasqueira granite and the formation of ore-bearing quartz veins by monitoring major and trace elements variations in quartz-white mica assemblages composing the two-mica granite, greisen and W–Sn-bearing quartz veins. The greisen is characterized by an overall depletion in Mg, Ti, Ca, Na, Ba, Sr, REE and enrichment in Fe, Li, Rb, Cs, Sn, W which reflect the breakdown of feldspars and fluid-rock interactions with W–Sn-bearing fluids. White-mica from greisen and mineralized quartz veins are enriched in granophile elements (F, Rb, Cs, Li, Sn, W and Zn) compared to magmatic muscovite from the two-mica granite. Trace elements contents in quartz depict trends which show the progressive enrichment in Ge and B and depletion in Al, Ti and Li from magmatic to hydrothermal quartz that emphasize the progressive evolution and cooling of the magmatic-hydrothermal system of Panasqueira. Geochemical similarities between quartz-white mica assemblages from greisen and wolframite-bearing veins suggest that greisenization and the formation of mineralized veins result from the same hydrothermal event and derived from the same source of hydrothermal fluids. Apatite from greisen and quartz vein yielded U–Pb ages of 292 ± 10 Ma and 295 ± 5 Ma respectively confirming that greisenization and the formation of mineralized veins occurred roughly at the same time. These ages also overlap with the emplacement age of the Panasqueira granite (296 ± 4 Ma), indicating a temporal link between greisenization, W–Sn mineralization and granite crystallization. Temperatures of the magmatic-hydrothermal system constrained by Ti-in quartz thermometry depicts a cooling trend from magmatic quartz of granite (700–600 °C) to hydrothermal quartz of greisen (500–400 °C) and veins (450–350 °C). These results suggest that greisenization and the formation of W–Sn bearing quartz veins occurred at the magmatic-hydrothermal transition, during which orthomagmatic fluids rich in volatils, incompatible elements and W–Sn were exsolved during the final solidification stage of the Panasqueira two-mica granite.

Published
2021
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20. Stepwise hydration of [CH3COOMg]+ studied by cold ion trap infrared spectroscopy: insights into interactions in the magnesium channel selection filters.

Author

Takayanagi, Hikaru, Bardaud, Jean-Xavier, Hirata, Keisuke, Brenner, Valérie, Gloaguen, Eric, Ishiuchi, Shun-ichi, and Fujii, Masaaki

Abstract

The magnesium channel controls Mg2+ concentration in the cell and plays an indispensable role in biological functions. The crystal structure of the Magnesium Transport E channel suggested that Mg2+ hydrated by 6 water molecules is transported through a selection filter consisting of COO− groups on two Asp residues. This Mg2+ motion implies successive pairing with −OOC-R and dissociation mediated by water molecules. For another divalent ion, however, it is known that RCOO−⋯Ca2+ cannot be separated even with 12 water molecules. From this discrepancy, we probe the structure of Mg2+(CH3COO−)(H2O)4–17 clusters by measuring the infrared spectra and monitoring the vibrational frequencies of COO− with the help of quantum chemistry calculations. The hydration by (H2O)6 is not enough to induce ion separation, and partially-separated or separated pairs are formed from 10 water molecules at least. These results suggest that the ion separation between Mg2+ and carboxylate ions in the selection-filter of the MgtE channel not only results from water molecules in their first hydration shell, but also from additional factors including water molecules and protein groups in the second solvation shell of Mg2+. [ABSTRACT FROM AUTHOR]

Published
2023
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26. Evaluation of antimony availability in a mining context: Impact for the environment, and for mineral exploration and exploitation.

Author

Esbrí, José María, primary, Minang, Carmelo M., additional, Rivera, Sofía, additional, Madrid-Illescas, Mercedes, additional, García-Noguero, Eva, additional, González-Valoys, Ana, additional, Maguregui, Maite, additional, Thouin, Hugues, additional, Battaglia-Brunet, Fabienne, additional, Gloaguen, Eric, additional, and Higueras, Pablo León, additional

Published
2023
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30. A Sb ± Au mineralizing peak at 360 Ma in the Variscan belt

Author

Pochon Anthony, Branquet Yannick, Gloaguen Eric, Ruffet Gilles, Poujol Marc, Boulvais Philippe, Gumiaux Charles, Cagnard Florence, Baele Jean-Marc, Kéré Inoussa, and Gapais Denis

Subjects
Sb ± Au mineralization, Armorican Massif, 40Ar/39Ar dating, tobelite, Geology, QE1-996.5
Abstract

40Ar/39Ar absolute dating on tobelite (an ammonium-rich white mica) has been performed in order to provide geochronological constraints on the Sb ± Au mineralization and hydrothermalism at the Saint-Aubin-des-Châteaux base metal-Sb ± Au occurrence (Variscan Central Armorican Domain, France). The results show that the Sb ± Au deposition occurred at ca. 360 Ma. Coupled with recent results obtained in neighboring areas, this occurrence seems to belong to a large-scale Early Carboniferous economic Sb ± Au mineralizing peak in the southeastern part of the Central Armorican Domain. The emplacement of a coeval widespread mafic magmatism in the region appears to represent a major trigger for this mineralizing system at shallow depths (less than 3 km). In the light of these new data, this Early Carboniferous mafic magmatic event must be considered for the overall understanding of the genesis of mineralizing systems at the scale of the whole Variscan belt. Finally, at Saint-Aubin-des-Châteaux, evidence of an Early Permian hydrothermal event is also reported through LA-ICP-MS U-Pb dating of fluorapatite, arguing for the re-use and re-opening of Early Carboniferous mineralizing plumbing system by late (i.e. Permian) fluid flow pulses although no metal mobilization was associated with this event.

Published
2019
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32. GeoERA Raw Materials Monograph : the past and the future

Author

Wittenberg, Antje, de Oliveira, Daniel Pipa Soares, Flindt Jørgensen, Lisbeth, González, Javier, Heldal, Tom, Aasly, Kari Aslaksen, Deady, Eimear, Kumelj, Špela, Horvath, Zoltan, McGrath, Eoin, Ferreira, Maria João, Calabaça, Teresa, Arvanitidis, Nikolaos, Sadeghi, Martiya, Bertrand, Guillaume, Gloaguen, Eric, Decree, Sophie, Gautneb, Håvard, Törmänen, Tuomo, Reginiussen, Helge, Sievers, Henrike, Quental, Lídia, Pereira, Aurete, Medialdea, Teresa, Schiellerup, Henrik, Zananiri, Irene, Ferreira, Pedro Tavares, Somoza, Luis, Monteys, Xavier, Alcorn, Trevor, Marino, Egidio, Lobato, Ana Belén, Kuhn, Thomas, Nyberg, Johan, Malyuk, Boris, Magalhães, Vítor Hugo, Lunar, Rosario, Hein, J. R., Cherkashov, Georgy, Brown, Teresa, Cassard, Daniel, Urvois, Marc, Pedersen, Mikael, Schjøth, Frands, Tulstrup, Jørgen, Eilu, Pasi, Hokka, Janne, Simoni, Mark, Carvalho, Jorge, Laskaridis, Kostas, Dedić, Željko, Habimana, Cyprien, and Liinamaa-Dehls, Anne

Subjects
Domestic sources, Europe, Mineral resources, Raw materials, Supply chains
Abstract

GeoERA Minerals projects have produced data aimed at supporting Europe’s minerals sector and to assist the European Commission to realise its goals for raw materials. Data has been compiled on mineral occurrences and mineral provinces across Europe, in particular, areas with potential to host Critical Raw Materials. Anecdotal evidence from the minerals sector provides an indication of the likelihood of exploration leading to mine development. For every 1,000 mineral showings examined, only 100 may receive further exploration work and of those 100, only 10 may warrant more detailed sampling either through trenching, drilling or other means and of those 10 only 1 may proceed to an evaluation through a full feasibility study which itself has only 50% chance of being positive. Following this, any project for which a mine proposal is made must undergo a full evaluation and permitting by authorities including full public consultation. The proposal may or may not pass this scrutiny. In terms of a schedule, the generally accepted minimum time frame from discovery to production is 10 years and usually much more, up to 20 years. info:eu-repo/semantics/publishedVersion

Published
2022

33. Evaluation of antimony availability in a mining context: Impact for the environment, and for mineral exploration and exploitation

Author

Química analítica, Kimika analitikoa, Esbrí, José María, Minang, Carmelo M., Rivera, Sofía, Madrid-Illescas, M, García-Noguero, Eva, González-Valoys, Ana, Maguregui Hernando, Maite, Thouin, Hugues, Battaglia-Brunet, Fabienne, Gloaguen, Eric, León Higueras, Pablo, Química analítica, Kimika analitikoa, Esbrí, José María, Minang, Carmelo M., Rivera, Sofía, Madrid-Illescas, M, García-Noguero, Eva, González-Valoys, Ana, Maguregui Hernando, Maite, Thouin, Hugues, Battaglia-Brunet, Fabienne, Gloaguen, Eric, and León Higueras, Pablo

Abstract

This work aims to establish Sb mobility, its transfer to biota and its effect on soil health in a semi-arid climate. The results show the presence of stibnite (Sb2S3) as the main primary Sb compound, bindhemite (Pb2Sb2O6(O,OH)), and minor proportions of stibiconite (Sb3+(Sb5+)2O6(OH)) as oxidised Sb species. This research also observes very high total Sb contents in mining materials (max: 20,000 mg kg−1) and soils (400–3000 mg kg−1), with physical dispersion around mining materials restricted to 450 m. The soil-to-plant transfer is very low, (bioaccumulation factor: 0.0002–0.1520). Most Sb remains in a residual fraction (99.9%), a very low fraction is bound to Fe and Mn oxy-hydroxides or organic matter, and a negligible proportion of Sb is leachable. The higher Sb mobility rates has been found under oxidising conditions with a long contact time between solids and water. The main factors that explain the poor Sb mobility and dispersion in the mining area are the low annual rainfall rates that slow down the Sb mobilisation process and the scarce formation of oxidised Sb compounds. All these data suggest poor Sb (III) formation and a low toxicological risk in the area associated with past mining activities. The low mobility of Sb suggests advantages for future sustainable mining of such ore deposits in a semi-arid climate and is also indicative of the limitations of geochemical exploration in the search for new Sb deposits.

Published
2022

38. Predictivity modelling from multivariate environments coupling Disc-Based Association and Random Forest analyses

Author

Vella, Alex, Bertrand, Guillaume, Tourlière, Bruno, Gloaguen, Eric, Labbé, Vincent, Gumiaux, Charles, Sizaret, Stanislas, Vella, Alex, and tArgeting eU cRitical mEtals (Sb, W) and predictibility of Sb-As-Hg envirOnmentaL issuEs - - AUREOLE2019 - ANR-19-MIN2-0002 - ERA-MIN 2 - VALID

Subjects
[SDU.STU] Sciences of the Universe [physics]/Earth Sciences, [STAT.ML] Statistics [stat]/Machine Learning [stat.ML]
Abstract

Mineral prospectivity mapping (MPM) aims at outlining areas with the highest mineralization hosting likelihood. The outcome of data-driven MPM approach highly depend on the spatial resolution and precision of the input cartographic datasets. Besides, the geological map has the inherent specificity of displaying 3D structures on a 2D surface map view; some structural configurations can usually lead to a misestimation of the relative proportion of the geological units, the faults or other features displayed in the map. From the Cell-Based Association (CBA), we develop here a new approach – the “Disc-Based Association” (DBA) – analyzing neighboring associations of cartographic features. First, disks entities are generated over a regular node grid covering the study area. Each disk discretize the overlapped data layers by integrating their information into a multivariate spectrum. Then, a Random Forest (RF) predictive model classify the multivariate spectrum from both mineralized nodes (e.g. whose associated disk contain a mineralization) and nonmineralized ones. As mineral concentration processes are inherently rare natural phenomena, we argue that all nodes except the mineralized one can be regarded as non-mineralized and thus used in the classification process. Predictivity scores are computed over the area based on the multivariate spectrum classification. This approach could allow the identification of several signature spectra associated to mineralization; which could be interpreted as several distinct metallotects / mineralization processes forming deposits in the study area. To test and evaluate its consistency, this new methodology is applied to prospectivity mapping of Sb along the Ibero-Armorican Arc (Western European Variscan Range). We infer this new data-driven approach applied to natural cases will improve prospectivity mapping and automatic recognition of new metallotects while giving new insights on the genetic processes forming deposits

Published
2022

39. Relationships between lithium-rich intrusions and partial melting of metasediments: clues from the French variscan belt

Author

Gloaguen, Eric, Gumiaux, Charles, Millot, Romain, Guerrot, Catherine, Leopold Dit Offite, Floriane, Lete, Melanie, Michaud, Julie, Deveaud, Sarah, Melleton, Jérémie, Gourcerol, Blandine, Guillou-Frottier, Laurent, Institut des Sciences de la Terre d'Orléans - UMR7327 (ISTO), Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)-Observatoire des Sciences de l'Univers en région Centre (OSUC), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS), Bureau de Recherches Géologiques et Minières (BRGM) (BRGM), Géodynamique - UMR7327, Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)-Institut des Sciences de la Terre d'Orléans - UMR7327 (ISTO), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)-Observatoire des Sciences de l'Univers en région Centre (OSUC), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), and Eric, Gloaguen

Subjects
[SDU.STU.AG] Sciences of the Universe [physics]/Earth Sciences/Applied geology, partial melting, lithium, rare-metal pegmatites, french variscan belt, granites, [SDU.STU.AG]Sciences of the Universe [physics]/Earth Sciences/Applied geology
Abstract

International audience; Geological processes leading to lithium-rich rare metal (RM) pegmatites and granites remain poorly constrained. To acknowledge geological processes related to Li-rich melt generation, we applied complementary approaches in the Montagne Noire (MN) and in the Monts d’Ambazac (MA). In the MN, the mineralogy of pegmatite clusters depends of the nature of the migmatitic host rock. Geostatistical studies demonstrate that pegmatite clusters are scattered and do not appear randomly. Lithium isotopes tracing (7Li, ‰) show that the mineralized pegmatites are not fractionated and display likely a crustal signature. Rb/Sr dating on lepidolites shows that their emplacements are synchronous with regional partial melting. In MA, structural studies and 3D modelling suggest the presence of an anatectic dome masked by a granite. Geostatistic studies demonstrate that emplacement of pegmatite clusters are controlled by normal faulting. Lithium isotopes show that the mineralized pegmatites are not fractionated and have a crustal signature. Rb/Sr dating on lepidolites show that pegmatite emplacement postdates the granite emplacement.A compilation of RM intrusions in France has been conducted in the present work and shows that: i) they are usually located in or along antiformal structures; ii) the core of antiformal structures consists of migmatites, amphibolite-grade metasediments or anatectic granites; iii) RM granites are spatially associated with major faults; iv) Li-rich RM pegmatites are absent in the case of LP-HT partial melting. These results point to an anatectic origin of RM pegmatite fields with a strong tectonic control of the intrusions near migmatitic domes. Then, the presence of RM pegmatite indicates presence of an underlying partial melting zone which should be more distal in the case of a granite. Moreover, the absence of Li-rich intrusions in the case of LP melting conditions suggests that pressure has a key role in magma enrichment processes during partial melting.

Published
2021

43. Evaluation of Antimony Availability in a Mining Context: Impact for the Environment, and for Mineral Exploration and Exploitation

Author

Esbrí, José María, primary, Minang, Carmelo M., additional, Rivera, Sofía, additional, Madrid-Illescas, Mercedes, additional, García-Noguero, Eva, additional, González-Valoys, Ana, additional, Maguregui, Maite, additional, Thouin, Hugues, additional, Battaglia-Brunet, Fabienne, additional, Gloaguen, Eric, additional, and Higueras, Pablo León, additional

Published
2022
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45. Contributors

Author

Barboux, Philippe, primary, Belchí Lorente, Daniel, additional, Chagnes, Alexandre, additional, Christmann, Patrice, additional, Dolhem, Franck, additional, Ekberg, Christian, additional, Gaubicher, Joël, additional, Gloaguen, Eric, additional, Labbé, Jean-François, additional, Luong, Van T., additional, Mandil, Guillaume, additional, Melleton, Jérémie, additional, Petranikova, Martina, additional, Piantone, Patrice, additional, Poizot, Philippe, additional, Renault, Stéven, additional, Svecova, Lenka, additional, Światowska, Jolanta, additional, Thivel, Pierre-Xavier, additional, Tran, Tam, additional, and Zwolinski, Peggy, additional

Published
2015
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47. Provide INSPIRE-compliant harmonised data on deposits and prospects of natural graphite, lithium and cobalt : DELIVERABLE D5.6

Author

Gautneb, Håvard, Törmänen, Tuomo, Gloaguen, Eric, and Pereira, Aurete

Subjects
Recursos minerais, Sistemas de informação, INSPIRE, Base de dados, Europa
Abstract

D.5.6 is the last deliverable of the work package 5 of the FRAME project. The two previous deliverables D5.4 and the D5.5 report the deliverable of the final work package data and products. All these three deliverables are related to products and data where the main results are presented on the web only. D5.6 with the title: Provide INSPIRE-compliant harmonised data on deposits and prospects of natural graphite, lithium and cobalt aims to deliver the data collected by the work package, to the GeoEra consortium and to upload the raw data, as comma separated file (CSV) format, to the European Geological Data Infrastructure (EGDI). The CSV file can then be integrated and downloaded to be used individually or with other data sets and web applications. Data is harmonised according to INSPIRE data specifications as far as it is possible. Since the main product of this deliverable is the release of the raw data and its availability on the net, this deliverable will be very concise. N/A

Published
2021

48. Prospectivity maps of critical raw materials in Europe : DELIVERABLE D3.5

Author

Bertrand, Guillaume, Sadeghi, Martiya, Arvanitidis, Nikolaos, de Oliveira, Daniel Pipa Soares, Gautneb, Håvard, Gloaguen, Eric, Törmänen, Tuomo, Reginiussen, Helge, Decree, Sophie, Pereira, Aurete, and Quental, Lídia

Subjects
Recursos minerais, Depósitos minerais, Matérias-primas, Mapa, Europa
Abstract

Submitted by CV Deposit (cvuser@cienciavitae.pt) on 2021-09-13T11:50:35Z No. of bitstreams: 2 FRAME_D_3_5_final.pdf: 6439256 bytes, checksum: 303711d5cde1dc2cb8bc6882f333ea40 (MD5) package.zip: 6065868 bytes, checksum: 996115a909304f8b016820e737dbfc26 (MD5) Approved for entry into archive by Paula Candeias (paula.candeias@lneg.pt) on 2021-11-04T10:05:26Z (GMT) No. of bitstreams: 2 package.zip: 6065868 bytes, checksum: 996115a909304f8b016820e737dbfc26 (MD5) FRAME_D_3_5_final.pdf: 6439256 bytes, checksum: 303711d5cde1dc2cb8bc6882f333ea40 (MD5) Made available in DSpace on 2021-11-04T10:05:27Z (GMT). No. of bitstreams: 2 package.zip: 6065868 bytes, checksum: 996115a909304f8b016820e737dbfc26 (MD5) FRAME_D_3_5_final.pdf: 6439256 bytes, checksum: 303711d5cde1dc2cb8bc6882f333ea40 (MD5) Previous issue date: 2021-06 N/A

Published
2021

49. Relevant metallogenetic maps : DELIVERABLE D5.5

Author

Gautneb, Håvard, Gloaguen, Eric, Törmänen, Tuomo, Pereira, Aurete, and Sadeghi, Martiya

Subjects
Metalogénese, Recursos minerais, Depósitos minerais, Mapa, Europa
Abstract

Submitted by CV Deposit (cvuser@cienciavitae.pt) on 2021-09-13T11:48:15Z No. of bitstreams: 2 FRAME_D5.5_final.pdf: 468653 bytes, checksum: fa01c103e6b61cd80768a62ddcade543 (MD5) package.zip: 453344 bytes, checksum: 87ceb4faf30ba72419cc4688193ec666 (MD5) Approved for entry into archive by Paula Candeias (paula.candeias@lneg.pt) on 2021-11-03T16:03:11Z (GMT) No. of bitstreams: 2 package.zip: 453344 bytes, checksum: 87ceb4faf30ba72419cc4688193ec666 (MD5) FRAME_D5.5_final.pdf: 468653 bytes, checksum: fa01c103e6b61cd80768a62ddcade543 (MD5) Made available in DSpace on 2021-11-03T16:03:11Z (GMT). No. of bitstreams: 2 package.zip: 453344 bytes, checksum: 87ceb4faf30ba72419cc4688193ec666 (MD5) FRAME_D5.5_final.pdf: 468653 bytes, checksum: fa01c103e6b61cd80768a62ddcade543 (MD5) Previous issue date: 2021-05 N/A

Published
2021

50. Map of Cobalt, graphite, lithium deposits (including deposits where cobalt is a significant by product : DELIVERABLE D5.4

Author

Gautneb, Håvard, Gloaguen, Eric, Törmänen, Tuomo, Pereira, Aurete, and Sadeghi, Martiya

Subjects
Cobalto, Recursos minerais, Depósitos minerais, Mapa, Lítio, Europa
Abstract

Submitted by CV Deposit (cvuser@cienciavitae.pt) on 2021-09-13T11:47:13Z No. of bitstreams: 2 FRAME_D5.4_final.pdf: 590080 bytes, checksum: 5b38b8abf35d9ff8197bce62858171f2 (MD5) package.zip: 578708 bytes, checksum: ccd0f68836f2e6932e34cb7721681281 (MD5) Approved for entry into archive by Paula Candeias (paula.candeias@lneg.pt) on 2021-11-03T15:08:00Z (GMT) No. of bitstreams: 2 package.zip: 578708 bytes, checksum: ccd0f68836f2e6932e34cb7721681281 (MD5) FRAME_D5.4_final.pdf: 590080 bytes, checksum: 5b38b8abf35d9ff8197bce62858171f2 (MD5) Made available in DSpace on 2021-11-03T15:08:00Z (GMT). No. of bitstreams: 2 package.zip: 578708 bytes, checksum: ccd0f68836f2e6932e34cb7721681281 (MD5) FRAME_D5.4_final.pdf: 590080 bytes, checksum: 5b38b8abf35d9ff8197bce62858171f2 (MD5) Previous issue date: 2021-05 N/A

Published
2021

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