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 …

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 …

Abstract 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 …

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 …

The rift system in North East Coast-Mahanadi (NEC-MND) basins has been developed
during the separation of India and Antarctica, similar to those in Krishna-Godavari (KG) and …

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

This chapter presents a seismic section from the Cauvery Basin showing a series of rift fault
blocks with a shallow crustal detachment. The large fault propagates deeper and due to …