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Geophysical study of a seamount located on the continental margin of India

DRS at CSIR-National Institute of Oceanography

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Title Geophysical study of a seamount located on the continental margin of India
 
Creator Bhattacharya, G.C.
Subrahmanyam, V.
 
Description Bathymetric, magnetic, and gravity data obtained over a 2,464 m high seamount located in the Arabian Sea indicate that the seamount (inferred mean density = 2.65 gm/cc) extends for 1 km beneath the seafloor and is locally isostatically compensated. With a reversely magnetized upper part and normally magnetized base, the seamount was probably formEd. by at least two volcanic episodes. The base was formed during the Late Paleocene (ca. 58 Ma) while the Indian Plate was moving over the Reunion hotspot. A renewed period of volcanism, contemporaneous with the major changes in direction of Indian Plate motion during the early Oligocene (ca. 36 Ma) probably formed the cap.
 
Date 2009-05-12T10:25:29Z
2009-05-12T10:25:29Z
1991
 
Type Journal Article
 
Identifier Geo-Marine Letters, Vol.11; 71-78p.
http://drs.nio.org/drs/handle/2264/3249
 
Language en
 
Rights Copyright [1991]. All efforts have been made to respect the copyright to the best of our knowledge. Inadvertent omissions, if brought to our notice, stand for correction and withdrawal of document from this repository.
 
Publisher Springer