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Hydrothermal fault zones in the lower oceanic crust: An example from Wadi Gideah, Samail ophiolite, Oman
Hydrothermal circulation is a key process for chemical and isotopic exchange between the
solid Earth and oceans, and for the extraction of heat from newly accreted crust at mid-ocean …
solid Earth and oceans, and for the extraction of heat from newly accreted crust at mid-ocean …
[HTML][HTML] Characterization of the active fault deformation zone of the Chegualin Fault in the alluvial plain of southwestern Taiwan
C Ding, JJ Dong, M Le Béon, CC Lee, SK Ho… - Engineering …, 2024 - Elsevier
The activity of a cree** active fault poses significant challenges to engineering structures
due to surface deformation. Therefore, quantifying the strain concentration caused by an …
due to surface deformation. Therefore, quantifying the strain concentration caused by an …
Interrogating an along-strike variation in the evolution and rheology of a large continental strike-slip fault zone
WA Sullivan - Journal of Structural Geology, 2024 - Elsevier
Along-strike variations in lithology, temperature, fluid activity, etc. can induce rheological
changes in strike-slip faults that may be recorded by different fault rocks and fabrics. This …
changes in strike-slip faults that may be recorded by different fault rocks and fabrics. This …
Physical and mechanical rock properties of a heterogeneous volcano; the case of Mount Unzen, Japan
Volcanoes represent one of the most critical geological settings for hazard modelling due to
their propensity to both unpredictably erupt and collapse, even in times of quiescence …
their propensity to both unpredictably erupt and collapse, even in times of quiescence …
Mineralogy and structures below Deccan Traps: Evidences from scientific drilling in the Koyna seismogenic zone, India
We study the deformation features preserved in basement granitoids recovered by scientific
core drilling from an active seismic zone in the Koyna region, Deccan Traps, India. The …
core drilling from an active seismic zone in the Koyna region, Deccan Traps, India. The …
The Alpine Fault hangingwall viewed from within: Structural analysis of ultrasonic image logs in the DFDP‐2B borehole, New Zealand
Ultrasonic image logs acquired in the DFDP‐2B borehole yield the first continuous,
subsurface description of the transition from schist to mylonite in the hangingwall of the …
subsurface description of the transition from schist to mylonite in the hangingwall of the …
[HTML][HTML] Fault zone architecture of a large plate-bounding strike-slip fault: a case study from the Alpine Fault, New Zealand
Abstract New Zealand's Alpine Fault is a large, plate-bounding strike-slip fault, which
ruptures in large (M w> 8) earthquakes. We conducted field and laboratory analyses of fault …
ruptures in large (M w> 8) earthquakes. We conducted field and laboratory analyses of fault …
Controls on fault zone structure and brittle fracturing in the foliated hanging wall of the Alpine Fault
Three datasets are used to quantify fracture density, orientation, and fill in the foliated
hanging wall of the Alpine Fault:(1) X-ray computed tomography (CT) images of drill core …
hanging wall of the Alpine Fault:(1) X-ray computed tomography (CT) images of drill core …
In-situ physical and elastic properties of Archaean basement granitoids in the Koyna seismogenic zone, western India from 3 km downhole geophysical well logs …
The Koyna region in western India is characterized by recurrent artificial water reservoir
triggered seismicity since the impoundment of the Shivaji Sagar lake in 1962. Physical and …
triggered seismicity since the impoundment of the Shivaji Sagar lake in 1962. Physical and …
Elastic properties and seismic anisotropy across the Alpine Fault, New Zealand
Seismically detected low‐velocity zones are commonly associated with major crustal faults.
In order to accurately interpret these low‐velocity zones and understand processes that …
In order to accurately interpret these low‐velocity zones and understand processes that …