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Rajat Mazumder

Researcher at German University of Technology in Oman

Publications -  80
Citations -  2183

Rajat Mazumder is an academic researcher from German University of Technology in Oman. The author has contributed to research in topics: Craton & Sedimentary depositional environment. The author has an hindex of 24, co-authored 77 publications receiving 1825 citations. Previous affiliations of Rajat Mazumder include Curtin University & Shandong University of Science and Technology.

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Proterozoic sedimentation and volcanism in the Singhbhum crustal province, India and their implications

TL;DR: In the Proterozoic volcano-sedimentary succession comprising successively younger Dhanjori, Chaibasa, Dhalbhum, Dalma and Chandil Formations of the Singhbhum crustal province, India records sedimentation and volcanism in a rapidly changing tectonic scenario as discussed by the authors.
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Tidal rhythmites and their implications

TL;DR: In this paper, the authors reviewed the methodologies of extracting lunar orbital periods from ancient tidal rhythmites, the mathematics behind the use of tidalites, and their limitations and uncertainties.
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Evidence of Enriched, Hadean Mantle Reservoir from 4.2-4.0 Ga zircon xenocrysts from Paleoarchean TTGs of the Singhbhum Craton, Eastern India.

TL;DR: Time integrated ɛHf[t] compositional array of the Hadean xenocrysts indicates a mafic protolith with 176Lu/177Hf ratio of ∼0.019 that was reworked during ∼4.2-4.0 Ga, suggesting that separation of such an enriched reservoir from chondritic mantle took place at 4.2 Ga.
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The 2.7–2.0 Ga volcano-sedimentary record of Africa, India and Australia: evidence for global and local changes in sea level and continental freeboard

TL;DR: The 2.7-2.0-Ga volcano-sedimentary records of the African, Indian and Australian cratons indicate two broadly defined periods of extensive drowning of the emergent continental areas, concomitant with lowered freeboard as mentioned in this paper.
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A commentary on the tectono-sedimentary record of the pre-2.0 Ga continental growth of India vis-à-vis a possible pre-Gondwana Afro-Indian supercontinent

TL;DR: In this paper, an integrated chronicle of major events leading to the growth of the pre-2.0 Ga Indian Craton, which is the aim of this paper, is an essential requirement to constrain the possibility of Neoarchaean unification between Africa and India.