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Christopher A. J. Wibberley

Researcher at Total S.A.

Publications -  29
Citations -  2352

Christopher A. J. Wibberley is an academic researcher from Total S.A.. The author has contributed to research in topics: Fault (geology) & Cataclastic rock. The author has an hindex of 15, co-authored 23 publications receiving 2040 citations. Previous affiliations of Christopher A. J. Wibberley include University of Montpellier & Kyoto University.

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A review of recent developments concerning the structure, mechanics and fluid flow properties of fault zones

TL;DR: Fault zones and fault systems have a key role in the development of the Earth's crust and control the mechanics and fluid flow properties of the crust, and the architecture of sedimentary deposits in basins as discussed by the authors.
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Internal structure and permeability of major strike-slip fault zones: the Median Tectonic Line in Mie Prefecture, Southwest Japan

TL;DR: Fault permeability data from the Median Tectonic Line (MTL) in Mie Prefecture, Southwest Japan suggest that fault permeability models are currently too simplistic for such large structurally complex fault zones.
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Are feldspar-to-mica reactions necessarily reaction-softening processes in fault zones?

TL;DR: In this article, microstructural information and geochemical data from the fault rocks suggest that different muscovitisation reactions occurred at different times within the evolution of the fault zone, and each reaction had its own impact on fault rheology.
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Hydraulic diffusivity of fault gouge zones and implications for thermal pressurization during seismic slip

TL;DR: In this paper, the authors used laboratory-determined permeability and compressibility data for natural fault gouge samples from the Median Tectonic Line (MTL) to estimate hydraulic diffusivities in fault- gouge zones.
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A model of strain localization in porous sandstone as a function of tectonic setting, burial and material properties; new insight from Provence (southern France)

TL;DR: In this paper, the analysis of three cataclastic band sets from Provence (France) reveals that the band density, their conjugate angles, their ratio of shear displacement to compaction and the amount of cataclasis within the bands differ and can be expressed as functions of tectonic setting and petrophysical properties.