Temperature trends for reaction rates, hydrogen generation, and partitioning of iron during experimental serpentinization of olivine-Reference-Cited by-同舟云学术

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Temperature trends for reaction rates, hydrogen generation, and partitioning of iron during experimental serpentinization of olivine

Published:2016-05 Issue: Volume:181 Page:175-200
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

McCollom Thomas M.^ORCID,Klein Frieder,Robbins Mark,Moskowitz Bruce,Berquó Thelma S.,Jöns Niels,Bach Wolfgang,Templeton Alexis

Funder

U. S. National Science Foundation Marine Geology and Geophysics program

Hanse Wissenschaftskolleg

DFG-Research Center/Excellence Cluster “The Ocean in the Earth System”

NSF Division of Earth Science

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference85 articles.

1. Geochemistry of reduced gas related to serpentinization of the Zambales ophiolite, Philippines;Abrajano;Appl. Geochem.,1990

2. Compositional controls on vent fluids from ultramafic-hosted hydrothermal systems at mid-ocean ridges: an experimental study at 400°C, 500 bars;Allen;Geochim. Cosmochim. Acta,2003

3. Occurrence, composition and growth of polyhedral serpentine;Andreani;Eur. J. Mineral.,2008

4. μXANES study of iron redox state in serpentine during oceanic serpentinization;Andreani;Lithos,2013

5. Aluminum speeds up the hydrothermal alteration of olivine;Andreani;Am. Mineral.,2013

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