Seismic anisotropy, as a ubiquitous feature in the Earth's interior, could record the past
lithospheric deformation and map directly mantle flow within our planet, and thus becomes a …

The northeastern region of India is one of the six most seismically active convergent plate
tectonic areas in the world. The north–south convergence along the Indo-Tibetan Himalayan …

The present study focuses on the source localization and depth estimation of anisotropy
beneath the eastern Himalaya ranging from Nepal in the west to Eastern Himalayan …

Shear wave birefringence is a robust tool to infer the direction and strength of deformation in
the lithosphere and sub-lithospheric mantle. Situated at the north-eastern flank of the Indian …

Ongoing oblique convergence at the eastern margin of the Indo-Eurasian collision zone
provides a natural laboratory for studying the deformation and dynamics of subduction …

This study attempts to interrogate the upper mantle deformation pattern beneath the Kumaon-
Garhwal region, located in the western Himalaya, using shear wave splitting (SWS) analysis …

The present study produces very new SKKS splitting measurements from the Northeast
India, suggesting the region as tectonically more heterogeneous and complex in nature. It …

ABSTRACT The North-Eastern region of India has the distinction of being one of the most
seismically active and tectonically complex regions in the world. The region has periodically …

Estimation of source localization and central depth of anisotropy beneath an active seismic
region plays an important role in understanding the deformation mechanism and current …

Abstract Characterization of null splitting measurements obtained from nine broadband
stations from the northeast Indian region using core-refracted seismic phases suggests a …