N
Naresh Chandra Pant
Researcher at University of Delhi
Publications - 77
Citations - 1262
Naresh Chandra Pant is an academic researcher from University of Delhi. The author has contributed to research in topics: Metamorphism & Metamorphic rock. The author has an hindex of 17, co-authored 69 publications receiving 1024 citations. Previous affiliations of Naresh Chandra Pant include Indian Institute of Technology Kharagpur & Geological Survey of India.
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Growth of the Greater Indian Landmass and its assembly in Rodinia: Geochronological evidence from the Central Indian Tectonic Zone
TL;DR: The Sausar Mobile Belt at the southern margin of the Central Indian Tectonic Zone (CITZ) is a key unit in constraining the timing of continent-continent collision between the North and South Indian cratonic blocks.
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Lithostructural and chronological constraints for tectonic restoration of Proterozoic accretion in the Eastern Indian Precambrian shield
S. Rekha,Dewashish Upadhyay,Abhijit Bhattacharya,Ellen Kooijman,S. Goon,S. Mahato,Naresh Chandra Pant +6 more
TL;DR: In this article, the authors used laser ablation inductively coupled plasma mass spectrometry (LAMS) to estimate the ages of the Chottanagpur Gneiss Complex (CGC), the North Singhbhum Mobile Belt (NSMB) and the Singhbhem Craton (SC).
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∼1.6 Ga ultrahigh‐temperature granulite metamorphism in the Central Indian Tectonic Zone: insights from metamorphic reaction history, geothermobarometry and monazite chemical ages
TL;DR: In this paper, the authors present precise pressuretemperature and age constraints of ultra-high-temperature (UHT) metamorphism of the Bhandara-Balaghat granulite (BBG) domain at the southern margin of the Central Indian Tectonic Zone (CITZ).
Journal Article
Evidence for Pre-Grenvillian high-pressure granulite metamorphism from the northern margin of the Sausar mobile belt in Central India
TL;DR: In this paper, the authors show that the mafic granulite-felsic migmatite gneiss association preserves early structures and high-P (∼ 10.5 kbar at ∼ 775°C) granulites histories which appear to pre-date and bear no relation to ∼ 1000 Ma old Sausar orogeny.
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Neoarchean high-pressure margarite–phengitic muscovite–chlorite corona mantled corundum in quartz-free high-Mg, Al phlogopite–chlorite schists from the Bundelkhand craton, north central India
L. Saha,Naresh Chandra Pant,J. K. Pati,Dewashish Upadhyay,Dewashish Upadhyay,Jasper Berndt,Abhijit Bhattacharya,M. Satynarayanan +7 more
TL;DR: In this article, the sharp chemical gradients across the highly structured bi-layered corona are inferred to suggest that the corona-forming reactions were promoted by local grain-boundary-controlled thermodynamic instability as opposed to element transport by advective diffusion.