To address the question of the initiation and mechanisms involved in the process of
subduction zone formation, we explored most of the available evidence for the subduction …

During the past 15 years, numerous studies have reported not only ecological and climatic
changes at 6-8 Ma, but also the roughly concurrent onsets of tectonic processes in regions …

India collided with mainland Asia at 65 Ma. The pressure rose to 9-11 kbar in the collision
zone. As the Indian lithosphere bent down and its upper crust buckled up as an upwarp in …

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 …

The Indian Ocean Nodule Field (IONF) is significant from several points of view. Roughly
bordered by 10° S to 16° 30′ S and 72° E to 80° E and located within the Central Indian …

Active intraplate deformation of the India–Australia Plate is now being captured by far-field
global positioning system (GPS) measurements as well as measurements on a few islands …

The nature of the crust in the Laxmi Basin, western margin of India, is an uncertain issue;
more importantly, this has implications on paleogeographic reconstructions of the western …

Abstract Long-wavelength (100–300 km) folding in the central Indian Ocean associated with
the diffuse plate boundary separating the Indian, Australian, and Capricorn plates is Earth's …

Results obtained from compilation and reinterpretation of about 21,200 line km of
bathymetry, magnetic and satellite gravity data between 10° S to 10° N latitudes and 75 to …

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 …