Titlebook: Geological and Geo-Environmental Processes on Earth; Arun Kumar Shandilya,Vinod Kumar Singh,Chandra She Book 2021 The Editor(s) (if applic

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https://doi.org/10.1007/978-3-642-92290-9ographic Mission (SRTM) Digital Elevation Model (DEM) data were used to extract drainage, density and contour maps. The drainage of Sindh and its subwatersheds exhibiting dendritic pattern show mean bifurcation ratio ranging from 3.85 to 5.66. It reveals that the drainage flowing in hilly and dissec

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Geological and Geo-Environmental Processes on Earth978-981-16-4122-0Series ISSN 2365-0656 Series E-ISSN 2365-0664

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https://doi.org/10.1007/978-3-7091-7512-5oarchean (ca. 2.7 Ga) metamorphism is predetermined by accretion-collision events; metamorphic processes associated with 2.55–2.50 Ga subduction-accretion events are extremely poorly defined; the latest Paleoproterozoic (1.9–1.8 Ga) prehnite-pumpellyite-facies metamorphism is associated with rifting.

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https://doi.org/10.1007/978-3-658-17734-8ane, mostly consists of Neoarchean potassic granitoids with the visible role of sanukitoids, monzogranites, and granodiorites (TTG), while the Southern terrane consists of mostly Neoarchean potassic granitoids with a minor amount of schist complex, sanukitoids, TTG, and mafic–ultramafic layered and mafic intrusion.

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Metamorphism of the Central Bundelkhand Greenstone Complex of the Bundelkhand Craton, Indian Shield oarchean (ca. 2.7 Ga) metamorphism is predetermined by accretion-collision events; metamorphic processes associated with 2.55–2.50 Ga subduction-accretion events are extremely poorly defined; the latest Paleoproterozoic (1.9–1.8 Ga) prehnite-pumpellyite-facies metamorphism is associated with rifting.

Congestion

Tectonostratigraphic Terranes of the Bundelkhand Craton (Indian Shield)ane, mostly consists of Neoarchean potassic granitoids with the visible role of sanukitoids, monzogranites, and granodiorites (TTG), while the Southern terrane consists of mostly Neoarchean potassic granitoids with a minor amount of schist complex, sanukitoids, TTG, and mafic–ultramafic layered and mafic intrusion.