Mineral and chemical compositions of carbonates from the Lost Village hydrothermal field, Mid-Atlantic Ridge

DOI

During Cruise 50 of R/V Akademik Mstislav Keldysh on the south slope of the Atlantis massif (30°07'N, Middle Atlantic Ridge) an inactive hydrothermal field named Lost Village was discovered. This new field was composed of light carbonate rock and was located near the active Lost City hydrothermal field. Mineral associations of these fields were studied. A conclusion about participation of ocean water in changing of carbonate composition of the inactive hydrothermal field was made.

Supplement to: Dara, O M; Kuz'mina, Tatyana G; Lein, Alla Yu (2009): Mineral Associations of the Lost Village and Lost City hydrothermal fields in the North Atlantic. Translated from Okeanologiya, 2009, 49(5), 742-750, Oceanology, 49(5), 688-696

Identifier
DOI https://doi.org/10.1594/PANGAEA.767383
Related Identifier https://doi.org/10.1134/S0001437009050105
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.767383
Provenance
Creator Dara, O M; Kuz'mina, Tatyana G; Lein, Alla Yu
Publisher PANGAEA
Publication Year 2009
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Language English
Resource Type Supplementary Publication Series of Datasets; Collection
Format application/zip
Size 2 datasets
Discipline Earth System Research
Spatial Coverage (-42.117 LON, 30.117 LAT); Lost Village Field, Mid-Atlantic Ridge