Journal
OCEANOLOGY
Volume 49, Issue 5, Pages 688-696Publisher
MAIK NAUKA/INTERPERIODICA/SPRINGER
DOI: 10.1134/S0001437009050105
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- Russian Foundation for Basic Research [06-05-64078]
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During the 50th cruise of R/V Akademik Mstislav Keldysh, on the south slope of the Atlantis massif (30 degrees 07'N; the Middle Atlantic Ridge), an inactive hydrothermal field named the Lost Village was discovered. This new field was formed of light carbonate rock and was located near the active Lost City hydrothermal field. The mineralogical associations of these fields were studied. A conclusion about the participation the ocean water in the changing of the carbonate composition of the inactive hydrothermal field was reached.
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