S
Subhajit Sinha
Researcher at University of Calcutta
Publications - 23
Citations - 237
Subhajit Sinha is an academic researcher from University of Calcutta. The author has contributed to research in topics: Geology & Aggradation. The author has an hindex of 6, co-authored 17 publications receiving 181 citations. Previous affiliations of Subhajit Sinha include Wadia Institute of Himalayan Geology & Durgapur Government College.
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Late Cenozoic fluvial successions in northern and western India: an overview and synthesis
TL;DR: Palaeomagnetic studies reveal that fluvial architecture and styles of deposition were controlled by Himalayan tectonics as well as by major climatic fluctuations during the long (∼13 Ma) span of formation as mentioned in this paper.
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Sedimentologic and geomorphic studies on the Quaternary alluvial fan and terrace deposits along the Ganga exit
TL;DR: Sedimentologic and geomorphologic records of a section of the Ganga Valley in the tectonically active eastern part of the Dehra Dun were studied to understand the interaction of tectonics and climate during Late Pleistocene-Holocene as mentioned in this paper.
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Soft-sediment deformation structures from the Paleoproterozoic Damtha Group of Garhwal Lesser Himalaya, India
TL;DR: In this article, soft-sediment deformation (SSD) structures are observed in the Damtha Group in the Garhwal Lesser Himalaya for a lateral extent of over 110 kilometres in comparable litho-sections.
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Geochemistry of Neogene Siwalik mudstones along Punjab re-entrant, India : Implications for source-area weathering, provenance and tectonic setting
TL;DR: In this paper, the Siwalik succession was analyzed for major, trace and rare earth elements (REEs) used as a reliable proxy to evaluate lithological composition, source-area weathering, provenance and tectonic setting of the basin.
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Provenance and weathering history of Mesoproterozoic clastic sedimentary rocks from the basal Gulcheru Formation, Cuddapah Basin
TL;DR: Geochemical analysis for the Mesoproterozoic clastic sedimentary rocks of the basal Gulcheru Formation of the Cuddapah Basin in the Gugudu-Dadithota-Parnapalle-Palkonda region (extending atleast 40 km) have been performed to highlight their provenance and weathering history as discussed by the authors.