Titlebook: Geodynamic Evolution of the Indian Shield: Geophysical Aspects; Om Prakash Pandey Book 2020 Springer Nature Switzerland AG 2020 Seismogene

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Geodynamic and Geologic Evolution of Indian Continent: A Brief History,arried out in Deccan volcanic terrain, which is considered one of the largest flood basaltic provinces on the surface of the Earth. Historically, it has been associated with a moderate intraplate seismic activity, usually not found in stable continental regions. Such unusual characters are very well reflected in all the geophysical fields.

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Book 2020al studies, like seismic, seismological, gravity, magnetic, magnetotelluric and heat flow, carried out over the past five decades. Further, it discusses elastic and petrophysical properties of the Earth’s crust relevant to geological investigations. The book also shares latest findings on the geodyn

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https://doi.org/10.1007/978-3-662-42515-2in the world. It is associated with distinct geologic, geotectonic and magmatic signatures. Indian shield underwent large scale deformation and degeneration at crust and lithospheric mantle level, due to sustained thermo-geodynamic perturbations, specially during the Cretaceous period, when the Eart

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Malaria biliosa haemoglobinurica,d active mobile belts. More than four decades ago, it was postulated through some studies that the Indian shield does not possess characteristics of a typical stable shield terrain. Out of these two cratons, Singhbhum craton, is perhaps the finest example of that, which forms one of the most deforme

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Rekurrensimpfbehandlung der Paralyse,ontinental shields and platform areas world-wide. Indian subcontinent contains four of them. All these basins came into existence due to sustained rifting and subsidence of the central part of the Indian peninsular shield. Out of these, the Vindhyan basin, located in central India and containing thi

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