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Fault zone fabric and fault weakness

Nature, 2009
Geological and geophysical evidence suggests that some crustal faults are weak compared to laboratory measurements of frictional strength. Explanations for fault weakness include the presence of weak minerals, high fluid pressures within the fault core and dynamic processes such as normal stress reduction, acoustic fluidization or extreme weakening at ...
Collettini   +7 more
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Fault zone hydrogeology

Earth-Science Reviews, 2013
article i nfo Deformation along faults in the shallow crust (b1 km) introduces permeability heterogeneity and anisotropy, which has animportantimpacton processes such asregional groundwater flow,hydrocarbon migration,andhy- drothermal fluid circulation.
Bense, V., F.   +4 more
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Discontinuous fault zones

Journal of Structural Geology, 1987
Abstract Many tectonic faults and tension fractures are, at least initially, composed of separate segments. This note deals with a little explored reason for this phenomenon which, in faulting, has obvious implications both for the migration of hydrocarbons and for the sealing capacity of faults. Theoretical arguments based on CoulombMohr's theory of
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