Titlebook: Geochemical Treasures and Petrogenetic Processes; John S. Armstrong-Altrin,Kailasa Pandarinath,Sanje Book 2022 The Editor(s) (if applicabl

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R. Stücker,W. Konermann,G. U. Exnerhanashini estuaries, along the central western coast of India, were investigated to understand the source, processes, and depositional environments. The distribution and abundance of parameters studied reveal that they were controlled largely by the catchment area geology, geomorphology, and estuari

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,Periartikuläre Verknöcherungen,057 m, ~3542 m, ~3726 m, and ~3738 m water depth, respectively). The grain size, mineralogy, geochemistry, and radiocarbon ages of the sediment cores were analyzed. N57 and N59 cores were characterized by detrital components enriched in SiO., Al.O., and Fe.O. contents. On the other hand, the N60, N6

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Portal und Multi-Provider-Managementestigation of the Paleogene glauconites in India. The biostratigraphic data reflects the overlapping temporal distribution of the Paleogene glauconitic rocks of Kutch, Cambay, Jaisalmer, Barmer, and Assam-Arakan basins, viz. late Paleocene-early Eocene, middle Eocene, and late Oligocene. In sharp co

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https://doi.org/10.1007/978-3-7091-4020-8n the localities of Sierra Anibacachi and Rancho Bufalo in northeastern Sonora to infer origin and source rocks type of their sediments. Zircon grains show large variations in P, Ti, Y, U, Th and Hf concentrations, while ΣREE concentrations in zircons vary significant from sample to sample. Zircon c

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