Brittle versus ductile deformation as the main control of the deep fluid circulation in oceanic crust

Author:

Violay M.1,Gibert B.2,Mainprice D.2,Burg J.-P.1

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

Reference35 articles.

1. Albertsson , A. J. O. Bjarnason T. Gunnarsson C. Ballzus K. Ingason 2003 The Iceland Deep Drilling Project: Fluid handling evaluation and utilization

2. High temperature instruments and methods developed for supercritical geothermal reservoir characterisation and exploitation-The Hiti Project;Asmundsson;Geothermics,2014

3. Permeability, porosity and pore geometry of hot pressed calcite;Bernabé;Mech. Mater.,1982

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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