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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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发表于 2025-3-21 18:49:46 | 显示全部楼层 |阅读模式
书目名称Geological Evolution of the Precambrian Indian Shield
编辑M.E.A. Mondal
视频videohttp://file.papertrans.cn/384/383318/383318.mp4
概述Presents the latest research on the Precambrian evolution of the Indian shield.Covers various aspects of geosciences, including paleobiology.Includes comprehensive petrological and geochemical dataset
丛书名称Society of Earth Scientists Series
图书封面Titlebook: Geological Evolution of the Precambrian Indian Shield; M.E.A. Mondal Book 2019 Springer International Publishing AG, part of Springer Natu
描述.This book presents findings from research into the Precambrian history of the Indian shield obtained using state-of-the-art technology. It demonstrates a paradigm shift towards studying the Precambrian shield regions using petrological, geochemical, structural, metallogenic, sedimentological and paleobiological data from the rocks in the Precambrian shield area, and presents a collection of contributions on these diverse topics that help to reconstruct the Precambrian evolution of the Indian Shield..
出版日期Book 2019
关键词Precambrian Sedimentary Basins; Phanerozoic reconstitution; Proto-Indian; Jahazpur granite; Break-up of
版次1
doihttps://doi.org/10.1007/978-3-319-89698-4
isbn_softcover978-3-030-07835-5
isbn_ebook978-3-319-89698-4Series ISSN 2194-9204 Series E-ISSN 2194-9212
issn_series 2194-9204
copyrightSpringer International Publishing AG, part of Springer Nature 2019
The information of publication is updating

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,Zircon U–Pb (SHRIMP) Ages of the Jahazpur Granite and Mangalwar Gneiss from the Deoli-Jahazpur Sectgranite. Concomitant metamorphism and granitic magmatism imply that overlying Hindoli-Jahazpur Group is younger than c. 2520 Ma. Thus, the Neoarchean Jahazpur granite and Mangalwar gneiss are constituents of the Banded Gneissic Complex which forms the basement of the Hindoli-Jahazpur supracrustal sequence.
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,Geochemistry of Mafic–Felsic Rocks of Phulad Ophiolite, in and Around Pindwara-Mount Abu Region, Sosent and well preserved in the area. With the help of systematic field mapping, a complete sequence has been reconstructed. New geochemical data in conjunction with published data affirms fore arc tectonic setting of this sequence.
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Book 2019leobiological data from the rocks in the Precambrian shield area, and presents a collection of contributions on these diverse topics that help to reconstruct the Precambrian evolution of the Indian Shield..
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https://doi.org/10.1007/978-3-030-55400-2ian crustal blocks which together constituted the Proto-India include Dharwar, Bastar, Singhbhum, Rajmahal, Bundelkhand, and Aravalli. The Protocontinents are separated from each other by Joins marked by Lineament like the Narmada-Son, or by the Gondwana rift basins like the Godavari, Mahanadi and t
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