Indian continental subduction can explain Cenozoic crustal deformation, magmatic activity
and uplift of the Tibetan Plateau following the India-Asia collision. In the western Himalayan …

We are able to decipher the tectonic evolution of the Bay of Bengal, a puzzle which has not
been satisfactorily solved in the past, and we are also able to shed new light on origin of the …

Analysis of new and existing geophysical data for the Central Indian and Wharton Basins of
the Indian Ocean were used to understand the formation and evolution of the Ninetyeast …

Continental transform margins are characterized by sub-vertical strike-slip faults and rapid
change in thermal gradient across the margin from continental to oceanic crust. The …

The present study used igneous provinces, mainly continental flood volcanics or oceanic
plateaus, at times associated with regional updoming, major rifting and continental breakup …

The sediment succession in the Bay of Bengal (BoB) records the signatures corresponding
to India–Asia collision, regional climate change, and erosional processes of both the …

Timing of breakup of the Indian continent from eastern Gondwanaland and evolution of the
lithosphere in the Bay of Bengal still remain as ambiguous issues. Geoid and free‐air gravity …

The convergence tectonics of the Ninetyeast Ridge (NER), upon the Andaman island arc–
trench system is examined through an analysis of ETOPO2 bathymetry, satellite-derived free …

The passive continental margins of India and conjugate Antarctica (30°–80° E) have been
reconstructed quantitatively by eliminating the intervening ocean floor. Recently acquired …

The formation of accretionary wedges with oversteepened slopes and uplifted axial zones
has been demonstrated to be potentially associated with highly oblique plate convergence …