Continental transform faults are dominantly highly localized strike-slip shear zones
hundreds of kilometers long that accumulate tens to hundreds of kilometers of displacement …

Abstract The Southern Alps of New Zealand are part of an active collisional orogen where
metamorphism, hydrothermal fluid flow and the formation of orogenic gold deposits are …

Magnetotelluric (MT) measurements along a profile cutting across the Garhwal Himalaya of
India are inverted to obtain 2-D electrical resistivity structures of the Himalayan wedge and …

An overview of seismicity along the northwest Himalaya exhibit along-strike segmentation
intricately controlled by the subsurface topographic ridges on the underthrusting Indian Plate …

Fluids residing in interconnected porosity networks have a significant weakening effect on
the rheology of rocks and can strongly influence deformation along fault zones. The …

The seismically active Saurashtra horst is located within the intraplate volcanic continental
margin of western India. The region is prone to moderate and low-magnitude earthquakes …

To determine the spatial distribution of earthquake potential along the active Himalayan arc,
we utilize GPS measurements and earthquake data. We derive horizontal velocity field and …

Fluids play a key role in modifying the chemical and physical properties of fault zones, which
may prime them for repeated rupture by the generation of high pore fluid pressures and …

Fluids play a prominent role in the genesis of earthquakes, particularly in intraplate settings.
In this study, we present evidence for a highly heterogeneous nature of electrical …

Metamorphic devolatilization generates fluids at, or near, lithostatic pressure. These fluids
are ultimately expelled by compaction. It is doubtful that fluid generation and compaction …