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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ATRIA

Crustal Evolution of Bundelkhand Craton in Archean and Comparison with Other Indian Cratonspt Singhbhum Craton) show that geodynamic mechanisms, similar to modern plate-tectonic and mantle-plume mechanisms, were active during Paleo-Neoarchean time. The Mesoarchean crustal evolution of the Bundelkhand Craton show subduction–accretion processes, which is different from other cratons of Indi

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Structure and Geological Processes of the Earth: Seismic Evidences from the Indian Shieldrface, whereas the external processes tend to destroy the shape of the Earth’s relief by weathering, erosion and hydrological cycle. The paper places the crustal structure of the Indian shield in the context of global processes and evolution of the Earth. It summarizes internal structure of the Eart

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Petrology and Geochemistry of Mafic–Ultramafic Rocks from Taka Area, Western Bastar Craton, Central aka village and adjoining areas of western Bastar craton, Central India. In the present study, we report petrological, mineralogical and geochemical data for these rocks. These data help to interpret the petrogenesis, composition of parental melt and their tectonic setting. These rocks are entirely

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Metamorphism of the Central Bundelkhand Greenstone Complex of the Bundelkhand Craton, Indian Shield cies; (2) ca. 2.7 Ga amphibolite-facies and metasomatism associated with its retrograde branch; (3) ca 1.9–1.8 Ga prehnite-pumpellyite-facies presumably associated with reef formation giant two-phase hydrothermal quartz veins. Data on the mineral associations, the chemical composition of minerals an

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Tectonostratigraphic Terranes of the Bundelkhand Craton (Indian Shield)ompose three tectonic divisions, i.e., the Northern, Central, and Southern Bundelkhand terranes of the craton. The Central terrane comprises Paleo- and Neo-archean tonalite–trondhjemite–granodiorite (TTG), greenstone sequences (ultrabasic-basic, felsic volcanites, Banded Iron Formation (BIF)), and N

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