The geodynamic evolution of the Tibetan Plateau remains highly debated. Any model of its
evolution must explain the plateau's growth as constrained by palaeo-altitude studies, the …

The topographic evolution of SE Tibet is essential for understanding the growth of this
orogenic plateau margin and the mechanism of continental deformation in general. Stable …

We develop a novel gravity inversion algorithm in spherical coordinates based on adaptive
inversion mesh refinement and multiphysical parameter constraints. The inversion mesh is …

The eastern Indian shield consists of Archaean Singhbhum Craton and Proterozoic
Chhotanagpur Gneissic Complex sandwiching the Singhbhum Mobile Belt. Since the …

Bastar craton located in the eastern part of the Indian shield is affected by multiple episodes
of mafic magmatism (mafic dyke swarms of∼ 1.9 Ga) and ultramafic kimberlite emplacement …

It is well known that the Tibetan plateau exposes a series of terranes that were drifted
northward and accreted progressively onto the south margin of Eurasia resulting from ocean …

A long-wavelength geoidal geometry characterizes the most pronounced features of the
Indian Ocean geoid low and the West Pacific and North Atlantic geoid highs. These large …

The underthrusting Indian plate beneath the Himalaya is considered to be segmented along
its arc which is manifested in terms of variations in the angle of underthrusting of the Indian …

Abstract The Cenozoic collision of India and Eurasia clearly built the high-elevation Tibetan
Plateau, but how this collision was accommodated, and the Tibetan Plateau uplifted …

The tectonic re-equilibration after the Variscan orogeny coincided with widespread early
Permian post-collisional magmatism in southern Europe. A full understanding of the origin of …