Morphotectonics of the Raman-Panikkar-Wadia seamount chain in the Laxmi Basin, Eastern Arabian Sea-Reference-Cited by-同舟云学术

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Morphotectonics of the Raman-Panikkar-Wadia seamount chain in the Laxmi Basin, Eastern Arabian Sea

Published:2024-03 Issue: Volume:262 Page:105977
ISSN:1367-9120
Container-title:Journal of Asian Earth Sciences
language:en
Short-container-title:Journal of Asian Earth Sciences

Author:

John Savio J.,Yatheesh V.,Bijesh C.M.,Mahender K.,Aswini K.K.,Badesab Firoz,Shuhail M.,Sriram G.,Twinkle D.,Kumar Raj

Funder

Council of Scientific and Industrial Research, India

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference48 articles.

1. Anilkumar, Pande, K., Venkatesan, T.R., Bhaskar Rao, Y.J., 2001. The Karnataka Late Cretaceous dykes as products of the Marion hotspot at the Madagascar - India breakup event: evidence from 40Ar/39Ar geochronology and geochemistry. Geophys. Res. Lett. 28, 2715-2718.

2. Early and late igneous pulses and high 3He plume origin for the Deccan Flood Basalts;Basu;Science,1993

3. Paleogeographic maps of the continents bordering the Indian Ocean since the Early Jurassic;Besse;J. Geophys. Res.,1988

4. Evidence for seafloor spreading in the Laxmi Basin, northeastern Arabian Sea;Bhattacharya;Earth Planet. Sci. Lett.,1994

5. Swath bathymetric investigation of the seamounts located in Laxmi Basin, Eastern Arabian Sea;Bhattacharya;Mar. Geod.,1994

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