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Hydrothermal mineral phases hosted in ankaramite basalts from lower part of the Taganana area. Mineralization consists of major jasper (quartz and opal) and celadonite, in association with minor hematite, magnetite, Fe Ca, Mg carbonates, Kaersutite, calcite. Mineral paragenesis and isotopic data re-ect submarine conditions of alteration.

Author

Frontiers

Language

EN