Brittle versus ductile deformation as the main control of the deep fluid circulation in oceanic crust
Author:
Affiliation:
1. D-ERDW; ETH; Zürich Switzerland
2. Geosciences Montpellier; Université de Montpellier-CC060; Montpellier France
Funder
ETH
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/2015GL063437/fullpdf
Reference35 articles.
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4. A non-linear rheology model for mid-ocean ridge axis topography;Chen;J. Geophys. Res.,1990
5. Brittle versus ductile deformation as the main control properties of low-porosity anhydrite rocks;De Paola;J. Geophys. Res.,2009
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