Geochemistry and Depositional Environment of Quartzites: Lower Cuddapah Supergroup, South India - Softcover
Synopsis
The Proterozoic sedimentary basins in India, in general, extend beyond Archaean cratonic basements disseminated over five main cratons. One such intracratonic sedimentary basin is known as the Cuddapah Basin which occurs in the eastern Dharwar craton. These sedimentary basins initiation or basin inversion is controlled by tectonic processes at the craton margins. The oldest sedimentation began ~1900 Ma ago as noticed in the Cuddapah Basin in the Eastern Dharwar craton with two cycles of sedimentation in the Paleoproterozoic roughly coinciding with global propagation in passive margin sedimentation. The Cuddapah Basin commences through the alluvial fan of the Gulcheru Quartzite with a basal polymict matrix to clast-supported conglomerate lying directly above the Archaean rocks. In line with above, this book describes the geochemical characters of the siliciclastic sediments of the Lower Cuddapah Supergroup. In addition, the field, petrographic and geochemical studies along with major, trace and rare earth elements were also described to understand the provenance characteristics of the source rocks.
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Geochemistry and Depositional Environment of Quartzites
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Scholars' Press Mrz 2020, 2020
ISBN 10: 6138923928
ISBN 13: 9786138923923
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Taschenbuch. Condition: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -The Proterozoic sedimentary basins in India, in general, extend beyond Archaean cratonic basements disseminated over five main cratons. One such intracratonic sedimentary basin is known as the Cuddapah Basin which occurs in the eastern Dharwar craton. These sedimentary basins initiation or basin inversion is controlled by tectonic processes at the craton margins. The oldest sedimentation began ~1900 Ma ago as noticed in the Cuddapah Basin in the Eastern Dharwar craton with two cycles of sedimentation in the Paleoproterozoic roughly coinciding with global propagation in passive margin sedimentation. The Cuddapah Basin commences through the alluvial fan of the Gulcheru Quartzite with a basal polymict matrix to clast-supported conglomerate lying directly above the Archaean rocks. In line with above, this book describes the geochemical characters of the siliciclastic sediments of the Lower Cuddapah Supergroup. In addition, the field, petrographic and geochemical studies along with major, trace and rare earth elements were also described to understand the provenance characteristics of the source rocks. 156 pp. Englisch. Seller Inventory # 9786138923923
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Geochemistry and Depositional Environment of Quartzites
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Condition: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Autor/Autorin: Ramanaiah SurasuraDr Surasura Ramanaiah is a Professor in the Department of Geology of S.V.University, Tirupati, A.P, India. His research interests have focused on exploration of georesources and applications of modern geotechniques . Seller Inventory # 385853844
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Geochemistry and Depositional Environment of Quartzites: Lower Cuddapah Supergroup, South India
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Geochemistry and Depositional Environment of Quartzites: Lower Cuddapah Supergroup, South India
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Geochemistry and Depositional Environment of Quartzites: Lower Cuddapah Supergroup, South India
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Geochemistry and Depositional Environment of Quartzites | Lower Cuddapah Supergroup, South India
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Taschenbuch. Condition: Neu. Geochemistry and Depositional Environment of Quartzites | Lower Cuddapah Supergroup, South India | Surasura Ramanaiah (u. a.) | Taschenbuch | Englisch | 2020 | Scholars' Press | EAN 9786138923923 | Verantwortliche Person für die EU: preigu GmbH & Co. KG, Lengericher Landstr. 19, 49078 Osnabrück, mail[at]preigu[dot]de | Anbieter: preigu. Seller Inventory # 118420213
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Geochemistry and Depositional Environment of Quartzites
Published by
Scholars' Press Mär 2020, 2020
ISBN 10: 6138923928
ISBN 13: 9786138923923
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Seller: buchversandmimpf2000, Emtmannsberg, BAYE, Germany
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Taschenbuch. Condition: Neu. This item is printed on demand - Print on Demand Titel. Neuware -The Proterozoic sedimentary basins in India, in general, extend beyond Archaean cratonic basements disseminated over five main cratons. One such intracratonic sedimentary basin is known as the Cuddapah Basin which occurs in the eastern Dharwar craton. These sedimentary basins initiation or basin inversion is controlled by tectonic processes at the craton margins. The oldest sedimentation began ~1900 Ma ago as noticed in the Cuddapah Basin in the Eastern Dharwar craton with two cycles of sedimentation in the Paleoproterozoic roughly coinciding with global propagation in passive margin sedimentation. The Cuddapah Basin commences through the alluvial fan of the Gulcheru Quartzite with a basal polymict matrix to clast-supported conglomerate lying directly above the Archaean rocks. In line with above, this book describes the geochemical characters of the siliciclastic sediments of the Lower Cuddapah Supergroup. In addition, the field, petrographic and geochemical studies along with major, trace and rare earth elements were also described to understand the provenance characteristics of the source rocks.VDM Verlag, Dudweiler Landstraße 99, 66123 Saarbrücken 156 pp. Englisch. Seller Inventory # 9786138923923
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Geochemistry and Depositional Environment of Quartzites : Lower Cuddapah Supergroup, South India
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Taschenbuch. Condition: Neu. nach der Bestellung gedruckt Neuware - Printed after ordering - The Proterozoic sedimentary basins in India, in general, extend beyond Archaean cratonic basements disseminated over five main cratons. One such intracratonic sedimentary basin is known as the Cuddapah Basin which occurs in the eastern Dharwar craton. These sedimentary basins initiation or basin inversion is controlled by tectonic processes at the craton margins. The oldest sedimentation began ~1900 Ma ago as noticed in the Cuddapah Basin in the Eastern Dharwar craton with two cycles of sedimentation in the Paleoproterozoic roughly coinciding with global propagation in passive margin sedimentation. The Cuddapah Basin commences through the alluvial fan of the Gulcheru Quartzite with a basal polymict matrix to clast-supported conglomerate lying directly above the Archaean rocks. In line with above, this book describes the geochemical characters of the siliciclastic sediments of the Lower Cuddapah Supergroup. In addition, the field, petrographic and geochemical studies along with major, trace and rare earth elements were also described to understand the provenance characteristics of the source rocks. Seller Inventory # 9786138923923
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Geochemistry and Depositional Environment of Quartzites: Lower Cuddapah Supergroup, South India
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paperback. Condition: New. NEW. SHIPS FROM MULTIPLE LOCATIONS. book. Seller Inventory # ERICA82361389239286