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Titlebook: Cratons and Fold Belts of India; Ram Sharma Book 2010 Springer-Verlag Berlin Heidelberg 2010 Cratons.Fold Belts.Geodynamic Models.Geology

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书目名称Cratons and Fold Belts of India
编辑Ram Sharma
视频videohttp://file.papertrans.cn/240/239326/239326.mp4
概述Includes supplementary material:
丛书名称Lecture Notes in Earth Sciences
图书封面Titlebook: Cratons and Fold Belts of India;  Ram Sharma Book 2010 Springer-Verlag Berlin Heidelberg 2010 Cratons.Fold Belts.Geodynamic Models.Geology
描述.Cratons and Fold Belts of India, is a unique attempt at presenting geological characteristics and evolution of the fold belts and the cratonic areas of the Indian shield. The author has evaluated the different evolutionary models for each fold belt in light of all the currently available geological and geochronological informations that are clearly listed. Shortcomings, if any, of each model are stated and a viable geodynamic model is presented for each fold belt. The book is self-contained – it includes an introduction to the processes of mountain building, especially plate tectonics theory with its application to the evolution of the Himalaya as an illustrative example – so that the reader can better appreciate the novel approach to the evolution of Proterozoic fold belts. The author eschews a detailed account of the fold belts for a clear description of all the concepts that go into building models. It is primarily written for graduate students, teachers and for those geoscientists who aspire to know all about the Indian shield..
出版日期Book 2010
关键词Cratons; Fold Belts; Geodynamic Models; Geology of India; Indian Shield; plate tectonics; tectonics
版次1
doihttps://doi.org/10.1007/978-3-642-01459-8
isbn_softcover978-3-642-26074-2
isbn_ebook978-3-642-01459-8Series ISSN 0930-0317 Series E-ISSN 1613-2580
issn_series 0930-0317
copyrightSpringer-Verlag Berlin Heidelberg 2010
The information of publication is updating

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Lecture Notes in Computer Sciencee cratonic areas of the Indian shield. The rocks making up the fold belts were the sediments derived from crustal rocks and volcanic material derived from the mantle, all deformed and metamorphosed during subsequent orogeny(s) brought about by collision of crustal plates (cratonic blocks) that are n
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Lecture Notes in Computer Sciencemargins are called continental arcs or Andean-type continental margins. The Andes is the simple orogenic belt that formed when oceanic lithosphere (Nazca plate) subducted eastward under a continental margin of South America.
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Precambrian Terrains and Mountain Building Processes,her fold belts as titled here, have rocks that were deformed and metamorphosed to varying degrees and intruded by plutonic bodies of granitic compositions. Some fold belts are also characterized by extensive thrust faulting and by movements along large transcurrent fault zones. Even extensional defo
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