Trace Element Geochemistry of Sulfides from the Ashadze-2 Hydrothermal Field (12°58′ N, Mid-Atlantic Ridge): Influence of Host Rocks, Formation Conditions or Seawater?

Trace Element Geochemistry of Sulfides from the Ashadze-2 Hydrothermal Field (12°58′ N, Mid-Atlantic Ridge): Influence of Host Rocks, Formation Conditions or Seawater?

The trace element (TS) composition of isocubanite, chalcopyrite, pyrite, bornite, and covellite from oxidized Cu-rich massive sulfides of the Ashadze-2 hydrothermal field (12°58′ N, Mid-Atlantic Ridge) is studied using LA-ICP-MS. The understanding of TE behavior, which depends on the formation condi...

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Bibliographic Details
Main Authors: Irina Melekestseva, Valery Maslennikov, Gennady Tret’yakov, Svetlana Maslennikova, Leonid Danyushevsky, Vasily Kotlyarov, Ross Large, Victor Beltenev, Pavel Khvorov
Format: Article
Language:English
Published: MDPI AG 2020-08-01
Series:Minerals
Subjects:
Ashadze-2 hydrothermal field
copper sulfides
formation conditions
LA-ICP-MS
Mid-Atlantic Ridge
mode of occurrence
Online Access:https://www.mdpi.com/2075-163X/10/9/743

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https://www.mdpi.com/2075-163X/10/9/743

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