Crustal evolution and sedimentation history of the Bay of Bengal since the Cretaceous

Author:

Rao D. Gopala,Krishna K. S.,Sar D.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference59 articles.

1. Signals of Barremian (116 Ma) or younger oceanic crust beneath the Bay of Bengal along 14°N latitude between 81°E and 93°E;Banerjee;Mar. Geol.,1995

2. Seismic reflection images of intraplate deformation, central Indian Ocean, and their tectonic significance;Bull;J. Geol. Soc. London,1992

3. Revised calibration of the geomagnetic polarity time scale for the late Cretaceous and Cenozoic;Cande;J. Geophys. Res.,1995

4. Marine geophysical studies over the 85°E Ridge, Bay of Bengal, in First International Seminar and Exhibition on “Exploration Geophysics in Nineteen Nineties”, Hyderabad, India;Chaubey;Extended Abstracts (AEG Publ.),1991

5. Himalayan uplift, sea level, and the record of Bengal Fan sedimentation at the ODP Leg 116 Sites;Cochran;Proc. Ocean Drilling Program Sci. Results.,1990

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