A NNW-SSE-trending graben in the inner shelf (40-60 m isobaths), a mid-shelf basement ridge (60-150 m isobaths), a shelf-margin basin (150-1000 m isobaths) and the Prathap Ridge Complex in the slope (1000-2000 m isobaths) extend as linear features along the southwestern continental margin of India between 12°20'N and 15°00'N. The basic structural framework of the margin seems to be influenced by the pre-existing Precambrian structural fabric of the continent. The mid-shelf basement ridge and the Prathap Ridge Complex are interpreted as manifestation of the rift-phase volcanism when India separated from Madagascar around 84 Ma
Abstract: Detailed geological field mapping has allowed the restoration of two full stratigraphic se...
Greater India's northern edge prior to collision with Asia is typically modelled as a rifted passive...
Peninsular India forms a keystone in Gondwana, linking the East African and Malagasy orogens with Ed...
Magnetic and bathymetric studies on the Konkan basin of the southwestern continental margin of India...
Analysis of the multi- and single beam bathymetric, seismic, magnetic and free-air gravity (ship-bor...
The present study contributes new constraints on, and definitions of, the reconstructed plate margin...
The chief elements in the structure of the earth's crust are shield and stable areas (platforms), se...
Results from detailed analyses of multi-channel seismic reflection data in association with gravity ...
A structural and lithological map has been produced covering the Spontang ophiolite and the north In...
The collision of India and Asia can be defined as a process that started with the closing of the Tet...
The Krishna-Godavari basin is a rifted passive margin basin that developed orthogonally to the NW-SE...
Multi-channel seismic reflection profiles across the southwest continental margin of India (SWCMI) s...
The western continental margin of India (WCMI) has evolved as a result of two-stage rifting and brea...
The collision of India and Asia can be defined as a process that started with the closing of the Tet...
The Cauvery-Palar basin is a major peri-cratonic rift basin located along the Eastern Continental Ma...
Abstract: Detailed geological field mapping has allowed the restoration of two full stratigraphic se...
Greater India's northern edge prior to collision with Asia is typically modelled as a rifted passive...
Peninsular India forms a keystone in Gondwana, linking the East African and Malagasy orogens with Ed...
Magnetic and bathymetric studies on the Konkan basin of the southwestern continental margin of India...
Analysis of the multi- and single beam bathymetric, seismic, magnetic and free-air gravity (ship-bor...
The present study contributes new constraints on, and definitions of, the reconstructed plate margin...
The chief elements in the structure of the earth's crust are shield and stable areas (platforms), se...
Results from detailed analyses of multi-channel seismic reflection data in association with gravity ...
A structural and lithological map has been produced covering the Spontang ophiolite and the north In...
The collision of India and Asia can be defined as a process that started with the closing of the Tet...
The Krishna-Godavari basin is a rifted passive margin basin that developed orthogonally to the NW-SE...
Multi-channel seismic reflection profiles across the southwest continental margin of India (SWCMI) s...
The western continental margin of India (WCMI) has evolved as a result of two-stage rifting and brea...
The collision of India and Asia can be defined as a process that started with the closing of the Tet...
The Cauvery-Palar basin is a major peri-cratonic rift basin located along the Eastern Continental Ma...
Abstract: Detailed geological field mapping has allowed the restoration of two full stratigraphic se...
Greater India's northern edge prior to collision with Asia is typically modelled as a rifted passive...
Peninsular India forms a keystone in Gondwana, linking the East African and Malagasy orogens with Ed...