Sulfide Formation as a Result of Sulfate Subduction into Silicate Mantle (Experimental Modeling under High P,T-Parameters)

Sulfide Formation as a Result of Sulfate Subduction into Silicate Mantle (Experimental Modeling under High P,T-Parameters)

Ca,Mg-sulfates are subduction-related sources of oxidized S-rich fluid under lithospheric mantle P,T-parameters. Experimental study, aimed at the modeling of scenarios of S-rich fluid generation as a result of desulfation and subsequent sulfide formation, was performed using a multi-anvil high-press...

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Bibliographic Details
Main Authors: Yuliya Bataleva, Yuri Palyanov, Yuri Borzdov
Format: Article
Language:English
Published: MDPI AG 2018-08-01
Series:Minerals
Subjects:
sulfate
S-rich fluid
sulfide
sulfidation
desulfation
high-pressure experiment
subduction
mantle metasomatism
lithospheric mantle
Online Access:http://www.mdpi.com/2075-163X/8/9/373

Internet

http://www.mdpi.com/2075-163X/8/9/373

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