Analyzing Fault Reactivation Behavior Using InSAR, Stress Inversion, and Field Observations During the 2025 Sındırgı Earthquake Sequence, Simav Fault Zone, Western Türkiye. [PDF]
Kutoğlu ŞH +4 more
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A numerical appraisal of the 'fault-valve' model of origin of lode-type gold deposits. [PDF]
Bhuyan S, Panigrahi MK.
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Integrating machine learning and geomorphic indices to assess tectonic geomorphology in the Karoun River Basin, Zagros, SW Iran. [PDF]
Khodabakhshnezhad A +5 more
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Forecasting the Largest Expected Earthquake in Canadian Seismogenic Zones. [PDF]
Thongmeesang K, Shcherbakov R.
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Geological conditions for shale gas accumulation and favorable zone evaluation in the Longmaxi formation of the Yanyuan Basin. [PDF]
Yong J +5 more
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Description, measurement and analysis of glacitectonically deformed sequences [PDF]
Lee, Jonathan R., Phillips, Emrys
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Wavelet-convolutional neural network for fault prediction in coal mine seismic data. [PDF]
Zou G, Han C, Yeh HG, Peng S.
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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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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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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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