Magnetic signatures of serpentinization at ophiolite complexes-Reference-Cited by-同舟云学术

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Magnetic signatures of serpentinization at ophiolite complexes

Published:2016-08 Issue:8 Volume:17 Page:2969-2986
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Bonnemains D.¹,Carlut J.¹,Escartín J.¹,Mével C.¹,Andreani M.²,Debret B.³

Affiliation:

1. Institut de Physique du Globe de Paris, Sorbonne Paris Cité, Univ. Paris Diderot, UMR 7154, CNRS; Paris France

2. Univ. Lyon, Université Lyon 1, ENS de Lyon, UMR 5276 LGL-TPE, CNRS; Villeurbanne France

3. Department of Earth Sciences; Durham University; Durham UK

Funder

Region Île-de-France SESAME

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2016GC006321/fullpdf

Reference76 articles.

1. Oxygen-isotope constraints on serpentinization processes in ultramafic rocks from the Mid-Atlantic Ridge (23°N)

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

3. Sulfur in serpentinized oceanic peridotites: Serpentinization processes and microbial sulfate reduction;Alt;J. Geophys. Res.,1998

4. Dynamic control on serpentine crystallization in veins: Constraints on hydration processes in oceanic peridotites;Andreani;Geochem. Geophys. Geosyst.,2007

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

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