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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Vydané v:	Journal of Earth System Science Ročník 129; číslo 1; s. 121
Hlavní autori:	Seshu, D, Lakshmi, M Prasanthi, Begum, S Parveen, Manglik, A
Médium:	Journal Article
Jazyk:	English
Vydavateľské údaje:	New Delhi Springer India 01.12.2020 Springer Nature B.V
Predmet:	Algorithms Curie temperature Depth Earth and Environmental Science Earth Sciences Geology Heated water Magnetic anomalies Magnetic intensity Modelling Plate tectonics Precambrian Quantitative research Shape Space Exploration and Astronautics Space Sciences (including Extraterrestrial Physics Thermal plumes Trends Velocity mafic intrusion Total magnetic intensity anomaly Cuddapah basin 2.5D modelling
ISSN:	2347-4327, 0253-4126, 0973-774X
On-line prístup:	Získať plný text
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