Fluid migration in faulted shale rocks: channeling below active faulting threshold-Reference-Cited by-同舟云学术

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Fluid migration in faulted shale rocks: channeling below active faulting threshold

Published:2020-05-15 Issue: Volume: Page:1-15
ISSN:1964-8189
Container-title:European Journal of Environmental and Civil Engineering
language:en
Short-container-title:European Journal of Environmental and Civil Engineering

Author:

Donzé Frédéric-Victor¹,Tsopela Alexandra¹,Guglielmi Yves²,Henry Pierre³,Gout Claude⁴

Affiliation:

1. Univ. Grenoble Alpes, Univ. Savoie Mont Blanc, CNRS, IRD, IFSTTAR, ISTerre, Grenoble, France;

2. Lawrence Berkeley National Laboratory, Earth and Environmental Science Area, Berkeley, CA;

3. CEREGE, Aix-Marseille University–CNRS–IRD, Marseille, France;

4. Total S.A, Pau, France

Publisher

Informa UK Limited

Subject

Civil and Structural Engineering,Environmental Engineering

Link

https://www.tandfonline.com/doi/pdf/10.1080/19648189.2020.1765200

Reference36 articles.

1. In situ and laboratory investigations of fluid flow through an argillaceous formation at different scales of space and time, Tournemire tunnel, southern France

2. Strength anisotropy of shales deformed under uppermost crustal conditions

3. Chlorine-36 data at Yucca Mountain: statistical tests of conceptual models for unsaturated-zone flow

4. Evaluation of Forchheimer equation coefficients for non-Darcy flow in deformable rough-walled fractures

5. The hydromechanical behaviour of a fracture: an in situ experimental case study

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