The Brittle‐Ductile Transition in Porous Limestone: Failure Mode, Constitutive Modeling of Inelastic Deformation and Strain Localization

Author:

Baud Patrick1ORCID,Hall Stephen23,Heap Michael J.1ORCID,Ji Yuntao45,Wong Teng‐fong6ORCID

Affiliation:

1. Université de Strasbourg CNRS Institut Terre et Environnement de Strasbourg Strasbourg France

2. Division of Solid Mechanics Lund University Lund Sweden

3. Lund Institute of Neutron and X‐ray Science Lund Sweden

4. State Key Laboratory of Earthquake Dynamics Institute of Geology Beijing China

5. HPT Laboratory Department of Earth Sciences Utrecht University Utrecht The Netherlands

6. Earth System Science Programme Faculty of Science The Chinese University of Hong Kong Hong Kong

Funder

Institut national des sciences de l'Univers

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference70 articles.

1. Compaction banding in high porosity carbonate rocks: 1. Experimental observations;Abdallah Y.;Journal of Geophysical Research: Solid Earth,2020

2. Compaction can limit peak vertical velocity at Yucca Mountain;Andrews D. J.;Eos, Transactions American Geophysical Union,2007

3. Fluid flow numerical experiments of faulted porous carbonates, Northwest Sicily (Italy)

4. Ductile flow in sub-volcanic carbonate basement as the main control for edifice stability: New experimental insights

5. Mechanical behavior, failure mode, and transport properties in a porous carbonate

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