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N. Ramesh Babu
Researcher at National Geophysical Research Institute
Publications - 5
Citations - 118
N. Ramesh Babu is an academic researcher from National Geophysical Research Institute. The author has contributed to research in topics: Craton & Mafic. The author has an hindex of 4, co-authored 5 publications receiving 73 citations. Previous affiliations of N. Ramesh Babu include Council of Scientific and Industrial Research.
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Paleomagnetic study of 1765 Ma dyke swarm from the Singhbhum Craton: Implications to the paleogeography of India
TL;DR: In this article, the authors reported the first key paleopole as a result of paleomagnetic study on a precisely dated 1765, which was used in this study to propose the paleogeographic reconstruction of India with Baltica Craton and North China Craton.
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A 2207 Ma radiating mafic dyke swarm from eastern Dharwar craton, Southern India: Drift history through Paleoproterozoic
TL;DR: This article reported new TE-TIMS precise Pb-Pb baddeleyite ages together with consistent paleomagnetic results on two Paleoproterozoic mafic dyke swarms, intruding Archean basement rocks in the northern and southern region of Cuddapah basin, Eastern Dharwar Craton.
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New paleomagnetic results on $$\sim $$ ∼ 2367 Ma Dharwar giant dyke swarm, Dharwar craton, southern India: implications for Paleoproterozoic continental reconstruction
TL;DR: In this paper, the authors reported new paleomagnetic results and precise paleopole position of the extensional study on the Dharwar dyke swarm in southern India, where they have sampled 29 sites on 12 dykes from NE-SW Karimnagar-Hyderabad dykes and Dhone-Gooty sector dykes.
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Pb–Pb baddeleyite ages of mafic dyke swarms from the Dharwar Craton: Implications for Paleoproterozoic LIPs and diamond potential of mantle keel
TL;DR: In this paper, the authors reported ten precise Pb-Pb TE-TIMS age determinations on baddeleyite grains separated from seven mafic dykes and three sills in the Eastern Dharwar craton.
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Baddeleyite PbPb geochronology and paleomagnetic poles for ~1.89–1.86 Ga mafic intrusions from the Dharwar craton, India, and their paleogeographic implications
TL;DR: A key paleomagnetic pole at 13°S, 152°E (k = 21, A95 = 7.8°) for recently identified 1864.7-Ma mafic magmatic event, based on a detailed study of dolerite dykes and sills intruding Archean basement rocks and Tadipatri formation of the Cuddapah basin, Dharwar craton respectively, was presented in this paper.