z-logo
open-access-imgOpen Access
Melting of peridotite and eclogite coexisting with reduced C-O-H fluid at 3-16 GPa: further constraints for redox melting models
Author(s) -
Konstantin D. Litasov,
Anton Shatskiy,
Eiji Ohtani
Publication year - 2019
Publication title -
international kimberlite conference extended abstracts: 2008
Language(s) - English
Resource type - Conference proceedings
DOI - 10.29173/ikc3686
Subject(s) - peridotite , eclogite , geology , partial melting , redox , geochemistry , thermodynamics , chemistry , inorganic chemistry , mantle (geology) , physics , paleontology , subduction , tectonics

The content you want is available to Zendy users.

Already have an account? Click here to sign in.
Having issues? You can contact us here
Accelerating Research

Address

John Eccles House
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom