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Tectonics of the Indian subcontinent
~
Banerjee, D. M.
Tectonics of the Indian subcontinent
Record Type:
Electronic resources : Monograph/item
Title/Author:
Tectonics of the Indian subcontinentby A. K. Jain, D. M. Banerjee, Vivek S. Kale.
Author:
Jain, A. K.
other author:
Banerjee, D. M.
Published:
Cham :Springer International Publishing :2020.
Description:
xxiii, 576 p. :ill., digital ;24 cm.
Contained By:
Springer eBooks
Subject:
Plate tectonicsSoutheast Asia.
Online resource:
https://doi.org/10.1007/978-3-030-42845-7
ISBN:
9783030428457$q(electronic bk.)
Tectonics of the Indian subcontinent
Jain, A. K.
Tectonics of the Indian subcontinent
[electronic resource] /by A. K. Jain, D. M. Banerjee, Vivek S. Kale. - Cham :Springer International Publishing :2020. - xxiii, 576 p. :ill., digital ;24 cm. - Society of earth scientists series,2194-9204. - Society of earth scientists series..
Tectonics of the Indian Sub-continent: An Introduction -- Indian Cratons -- Tectonics of Sri Lanka -- Proterozoic Mobile Belts -- Proterozoic 'Purana' Basins -- Tectonics of the Himalaya -- Trans-Himalayan and Karakoram ranges -- Deccan Volcanic Province -- Tectonics of Western Margin of India -- Geology and Tectonics of Bangladesh.
This books documents the salient characters of the tectonic evolution of the Indian subcontinent. It showcases the well investigated subcontinent of Gondwana. The book is linked to an updated geological and tectonic map of this region on 1:12,000,000 in scale. The Indian subcontinent displays almost uninterrupted and unique the geological history since about Eo-Archean (~3800 Ma) to recent, with the development of many Proterozoic deformed and metamorphosed fold belts around Archean nuclei, and enormously thick undeformed platform deposits. After their stabilization during late Proterozoic, the subcontinent underwent Paleozoic rifting and deposition of coal-bearing thick sequences, followed by enormously-thick outpouring of Deccan volcanics as a consequence of huge mantle plume. The youngest event in its evolution is the Cenozoic Himalayan Orogenic Mountains, spanning the area between Nanga Parbat and Namcha Barwah; a part of which extends both in Pakistan and Myanmar.
ISBN: 9783030428457$q(electronic bk.)
Standard No.: 10.1007/978-3-030-42845-7doiSubjects--Topical Terms:
858580
Plate tectonics
--Southeast Asia.
LC Class. No.: QE511.4 / .J356 2020
Dewey Class. No.: 551.136
Tectonics of the Indian subcontinent
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by A. K. Jain, D. M. Banerjee, Vivek S. Kale.
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2020.
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ill., digital ;
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2194-9204
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Tectonics of the Indian Sub-continent: An Introduction -- Indian Cratons -- Tectonics of Sri Lanka -- Proterozoic Mobile Belts -- Proterozoic 'Purana' Basins -- Tectonics of the Himalaya -- Trans-Himalayan and Karakoram ranges -- Deccan Volcanic Province -- Tectonics of Western Margin of India -- Geology and Tectonics of Bangladesh.
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This books documents the salient characters of the tectonic evolution of the Indian subcontinent. It showcases the well investigated subcontinent of Gondwana. The book is linked to an updated geological and tectonic map of this region on 1:12,000,000 in scale. The Indian subcontinent displays almost uninterrupted and unique the geological history since about Eo-Archean (~3800 Ma) to recent, with the development of many Proterozoic deformed and metamorphosed fold belts around Archean nuclei, and enormously thick undeformed platform deposits. After their stabilization during late Proterozoic, the subcontinent underwent Paleozoic rifting and deposition of coal-bearing thick sequences, followed by enormously-thick outpouring of Deccan volcanics as a consequence of huge mantle plume. The youngest event in its evolution is the Cenozoic Himalayan Orogenic Mountains, spanning the area between Nanga Parbat and Namcha Barwah; a part of which extends both in Pakistan and Myanmar.
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Southeast Asia.
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Banerjee, D. M.
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Kale, Vivek S.
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https://doi.org/10.1007/978-3-030-42845-7
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Earth and Environmental Science (Springer-11646)
based on 0 review(s)
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000000178472
電子館藏
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EB QE511.4 .J25 2020 2020
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1 records • Pages 1 •
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https://doi.org/10.1007/978-3-030-42845-7
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