The idea of a simple linear boundary between continental and oceanic crust at extended
continental margins is widely recognized to be an oversimplification. Despite this, such …

Published models for the Cretaceous seafloor‐spreading history of East Gondwana result in
unlikely tectonic scenarios for at least one of the plate boundaries involved and/or violate …

The available plate-tectonic evolution models suggest that the deep ocean basins adjoining
the western continental margin of India have evolved largely due to break-up and dispersal …

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 …

Cauvery Basin, a pericratonic rift basin along the Eastern Continental Margin of India,
evolved during the breakup of the Eastern Gondwanaland. It exposes both syn-rift and later …

The 85° E Ridge is a buried aseismic ridge running parallel to the 85° E meridian in the Bay
of Bengal, India. Its origin has been a subject of debate, with opinions ranging from an …

The Cauvery basin, an important Indian petroliferous peri-cratonic Mesozoic rift basin trends
NE. The basin formed by break-up of eastern Gondwana landmass in Late Jurassic to Early …

On the edge of our continents, oceanic crust meets continental crust. At passive margins,
those where there is no active tectonics, subduction or transform faulting, these crustal types …

Summary The Cauvery Basin, a pericratonic rift basin evolved during Jurassic to Early
Cretaceous time as the eastern Gondwanaland rifted. Transfer zones conserve the amount …

The study focuses on the flexural down-war** of oceanic crust related to the Early
Cretaceous hotspot volcanic chain in offshore East India, drawing from robust reflection …