Titlebook: Geological Evolution of the Precambrian Indian Shield; M.E.A. Mondal Book 2019 Springer International Publishing AG, part of Springer Natu

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Geological Evolution of the Precambrian Indian Shield

MELON

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Evolution of the Indian Shield: A New Approach,ravalli craton (AC), all comprising greenstone-gneiss in different abundance ratios. As in other Archean terrains, this ocean-continental rock association dichotomy is explained by extrusion of mafic lava and its transformation into greenstone along with its melting at depth to generate tonalitic ma

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,Zircon U–Pb (SHRIMP) Ages of the Jahazpur Granite and Mangalwar Gneiss from the Deoli-Jahazpur Secte Aravalli Craton, northwestern India. These data are useful to understand the stratigraphic correlation between the basement gneiss and the low-grade supracrustal rocks of the Hindoli-Jahazpur Group. U–Pb (SHRIMP-IIe) data from zircon suggest emplacement age of 2538?±?5?Ma for the Jahazpur granite,

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,Mineral Chemistry, Sr–Nd Isotope Geochemistry and Petrogenesis of the Granites of Bathani Volcano-Sgpur Granite Gneiss Complex of Central Indian Tectonic Zone has been presented in this paper to understand its petrogenesis and implications for crustal growth in the eastern Indian shield. Petrographically, they are coarse-grained granites with biotite, plagioclase feldspar and K-feldspar as major

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Stratigraphic Evolution and Architecture of the Terrestrial Succession at the Base of the Neoproteruilding pattern within the ambit of the Precambrian fluvial sedimentation system. Detailed facies, architectural element, paleocurrent as well as stratigraphic architectural analysis invariably revealed a frequently avulsive braided pattern, with flashy discharges, for the paleoriver system; which i

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Deformation and Tectonic History of Punagarh Basin in the Trans-Aravalli Terrane of North-Western Ieformed and metamorphosed basement rocks of Sojat Formation. The basement rocks were deformed into upright inclined folds with parallel to chevron geometry. The axial plane cleavages were developed showing variation in trend from NE-SW to ENE-WSW and this variation was due to late generation open fo