Characterizing the source of a prominent magnetic anomaly in the southwestern part of the Cuddapah basin

The total magnetic intensity anomaly (TMI) map of the Proterozoic intracratonic Cuddapah basin shows the presence of a prominent high–low–high anomaly of about 600 nT amplitude at its southern end. The source of this anomaly is inferred to be a mafic intrusive body due to a thermal plume that might...

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Bibliographic Details
Published in:Journal of Earth System Science Vol. 129; no. 1; p. 121
Main Authors: Seshu, D, Lakshmi, M Prasanthi, Begum, S Parveen, Manglik, A
Format: Journal Article
Language:English
Published: New Delhi Springer India 01.12.2020
Springer Nature B.V
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ISSN:2347-4327, 0253-4126, 0973-774X
Online Access:Get full text
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