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109 results on '"Cita M.B."'

1. Contributors

Author

Albertão, G.A., primary, Andrade, C., additional, Bourgeois, J., additional, Cita, M.B., additional, Costa, P.J.M., additional, Dawson, A.G., additional, Feist, L., additional, Fujino, S., additional, Fujiwara, O., additional, Goto, K., additional, Higman, B., additional, Ichihara, T., additional, Imamura, F., additional, Jarupongsakul, T., additional, Kamataki, T., additional, Keerthi, N., additional, Kunthasap, P., additional, Marini, F., additional, Martins, P.P., additional, Matsui, T., additional, Minoura, K., additional, Murayama, M., additional, Nanayama, F., additional, Naruse, H., additional, Nishimura, Y., additional, Reicherter, K., additional, Ruangrassamee, A., additional, Scheffers, A., additional, Shiki, T., additional, Stewart, I., additional, Sugawara, D., additional, Supharatid, S., additional, Suphawajruksakul, A., additional, Tachibana, T., additional, Tada, R., additional, Tajika, E., additional, Tsuji, Y., additional, and Yamazaki, T., additional

Published
2021
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5. CONTRIBUTORS

Author

Albertão, G.A., primary, Bourgeois, J., additional, Cita, M.B., additional, Dawson, A.G., additional, Fujino, S., additional, Fujiwara, O., additional, Goto, K., additional, Helsley, C.E., additional, Higman, B., additional, Ichihara, T., additional, Imamura, F., additional, Jarupongsakul, T., additional, Kamataki, T., additional, Keating, B.H., additional, Keerthi, N., additional, Kunthasap, P., additional, Marini, F., additional, Martins, P.P., additional, Matsui, T., additional, Minoura, K., additional, Murayama, M., additional, Nanayama, F., additional, Naruse, H., additional, Nishimura, Y., additional, Ruangrassamee, A., additional, Scheffers, A., additional, Shiki, T., additional, Stewart, I., additional, Sugawara, D., additional, Supharatid, S., additional, Suphawajruksakul, A., additional, Tachibana, T., additional, Tada, R., additional, Tajika, E., additional, Tsuji, Y., additional, Wanink, M., additional, and Yamazaki, T., additional

Published
2008
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22. History of the Mediterranean Salinity Crisis

Author

Hsu, K.J., primary, Montadert, L., additional, Bernoulli, D., additional, Cita, M.B., additional, Erikson, A., additional, Garrison, R.E., additional, Kidd, R.B., additional, Melieres, F., additional, Muller, C., additional, and Wright, R., additional

Published
1978
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34. Site 12

Author

Peterson, M.N.A., primary, Edgar, N.T., additional, von der Borch, C., additional, Cita, M.B., additional, Gartner, S., additional, Goll, R., additional, and Nigrini, C., additional

Published
1970
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36. Site 8

Author

Peterson, M.N.A., primary, Edgar, N.T., additional, von der Borch, C., additional, Cita, M.B., additional, Gartner, S., additional, Goll, R., additional, and Nigrini, C., additional

Published
1970
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38. Site 9

Author

Peterson, M.N.A., primary, Edgar, N.T., additional, von der Borch, C., additional, Cita, M.B., additional, Gartner, S., additional, Goll, R., additional, and Nigrini, C., additional

Published
1970
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46. Sedimentation and formation of secondary minerals in the hypersaline Discovery Basin, eastern Mediterranean

Author

Wallmann K. 1, Aghib F.S. 2, Castradori D. 3, Cita M.B. 4, Suess E. 5, Greinert J. 6, and Rickert D. 7

Subjects
hypersaline brines, Discover Basin, secondary minerals, carbonates and sulfates
Abstract

Two cores recovered from the Discovery Basin and one reference core from a location outside the Basin were investigated in detail in order to decipher the influence of hypersaline brines on sediment geochemistry. The cores contain a tephra layer (presumable Y-5) and carbonate microfossils which permit a tentative chrono- and lithostratigraphic correlation. A layer containing up to 60 wt% biogenic opal and 6.6 wt% organic carbon was identified in one basin core, which probably represents the best preserved example of eastern Mediterranean sapropel S-1. The basin is filled with a concentrated solution of MgCl2 which is enriched in dissolved sulfate and has the highest salinity ever encountered in the marine environment. Pore water profiles demonstrate that this brine dissolves sedimentary calcite to form secondary carbonate- and sulfate-bearing minerals. Of these, dolomite, magnesite and gypsum were identified by X-ray diffractometry; thermodynamic calculations show that these phases form in equilibrium with the anomalous brine composition.

Published
2002

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