During the late Oligocene–early Miocene there were several major geological events in and
around the Tibetan Plateau (TP). First, crustal shortening deformation ceased completely …

Abstract The Bengal Basin is a collisional foreland basin in South Asia located at the
juncture of the Eurasian, Indian and Burmese Plates occupying Bangladesh and parts of the …

The Indian subcontinent comprises accreted cratonic fragments that underwent subsequent
rifting–subduction–collision processes along major mobile belts. It is also a storehouse of a …

An understanding of the sedimentary and crustal structure of the Bengal Basin and of the
tectonics deforming it remains elusive due to lack of seismic data from Bangladesh. Taking …

We present a new thermal and strength model for the lithosphere of Mainland China. To this
purpose, we integrate a thermal model for the crust, using a 3‐D steady state heat …

The persistence of significant topography in ancient, tectonically inactive orogenic belts
remains one of the outstanding questions in geomorphology. In southern Peninsular India …

The Indian subcontinent is a repository of Archean cratonic nuclei with plethora of
geoscientific data to better understand the early Earth evolution and the operating …

Significant diversity in the Indian lithosphere is seen in 3-D shear wave velocity images
inverted from the dispersion of group velocities measured from ambient noise and …

It is generally accepted that the subduction polarity reversal (SPR) results from the strong
collision of two plates. Yet, the SPR of the Solomon Back‐arc Basin is started in the “soft …

The present study attempts a conjugate analysis of satellite-based remote sensing, gravity,
and magnetic data for evaluation of structures and tectonic for new insights on Kimberlite …