Results 251 to 260 of about 320,218 (310)
Unveiling earthquakes: thermoluminescence signal resetting of a natural polymineral sample in laboratory-produced fault gouge. [PDF]
Sci RepHeydari M +7 more
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A settingless fault detection approach for MVDC network. [PDF]
Sci RepKassem A +3 more
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Distribution patterns and formation mechanisms of stable landslide dams in the Qinghai-Tibet plateau: a preliminary study. [PDF]
Sci RepSong L, Ma L, Chang Z, Wang Y.
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Decoding the southeastern Tibetan Plateau growth: a 3D numerical simulation of Cenozoic crustal deformation. [PDF]
Natl Sci RevWang Y +5 more
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Fault zone fabric and fault weakness
Nature, 2009Geological 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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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.
Víctor F Bense, Tom Gleeson, O Bour
exaly +3 more sources
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.
Víctor F Bense, Tom Gleeson, O Bour
exaly +3 more sources
Granular Packings and Fault Zones
Physical Review Letters, 2000The failure of a two-dimensional packing of elastic grains is analyzed using a numerical model. The packing fails through formation of shear bands or faults. During failure there is a separation of the system into two grain-packing states. In a shear band, local "rotating bearings" are spontaneously formed.
, Astrom, , Herrmann, , Timonen
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Facies Modelling in Fault Zones
ECMOR X - 10th European Conference on the Mathematics of Oil Recovery, 2006Traditionally fault impact on fluid flow is included by assigning transmissibility multipliers to flow simulation grid cell faces co-located with the fault plane (Manzocchi et al. 1999). A new method, called Fault Facies modelling (Tveranger et al. 2004, 2005), captures fault impact by considering faults as deformed rock volumes rather than simple ...
Syversveen, Anne Rand +4 more
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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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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
openaire +2 more sources