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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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The Role of Complementary Protectionrred to be braided, channels possibly become more sinuous towards the top of the succession, as inferred from the appearance of bank-attached bars along with the omnipresent longitudidal bars. Flow durability within channel also increases with time, as the lower two belts appear to be ephemeral with
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https://doi.org/10.1007/978-3-030-50597-4 TTG exhibit: (i) highly fractionated rare earth element (REE) patterns; and (ii) negative anomalies of Nb and Ti. These geochemical characteristics of the TTG suggest that they were not produced from partial melting of mid-oceanic ridge basalts/normal oceanic crust. Instead we propose that the TTG
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International Law in the Western Hemisphereical, fluidal and alterational characteristics closely resembling IOCG settings. Their timing and other similarities possibly indicate a major crustal scale event of brecciation associated with ascent of magmatically derived hydrothermal fluids and extensive epithermal alteration of host rocks. Thes
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