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Book Cover
E-book
Author Jain, A. K. (Arvind K.)

Title Tectonics of the Indian Subcontinent / A.K. Jain, D.M. Banerjee, Vivek S. Kale
Published Cham : Springer, 2020

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Description 1 online resource (594 pages)
Series Society of Earth Scientists Ser
Society of Earth Scientists series.
Contents Intro -- Series Editor Foreword -- Preface -- References -- Contents -- About the Authors -- 1 Tectonics of the Indian Subcontinent: An Introduction -- 1.1 Introduction -- 1.2 Peninsular India -- 1.2.1 Mountains and Plateaus -- 1.2.2 Coastal Plains -- 1.2.3 Himalaya -- 1.2.4 Indus-Ganga-Brahmputra Plain -- 1.3 Geology and Tectonics -- 1.3.1 Ancient Cratons -- 1.3.2 Proterozoic Mobile Belts -- 1.3.3 Intracratonic Sedimentary Basins -- 1.3.4 Himalaya Mobile Belt -- 1.3.5 Andaman Island Arc and Central Myanmar Plain -- References -- 2 Indian Cratons -- 2.1 Introduction -- 2.2 Aravalli Craton
2.2.1 Geological Framework -- 2.2.2 Banded Gneissic Complex (BGC) -- 2.2.3 Tectonothermal Events and Metamorphism in Sandmata and Mangalwar Complexes -- 2.2.4 Sedimentation Over the Rifted Aravalli Basement -- 2.2.5 Nature of Tectonic Contacts -- 2.2.6 Volcano-Sedimentary Greenstone Belts -- 2.2.7 The Berach Granite-Base of the Aravalli Metasediments -- 2.2.8 The Mangalwar Complex: The Sequence Above -- 2.2.9 Place in the Global Paleogeography -- 2.3 Bundelkhand Craton -- 2.3.1 Spatial Distribution and Geological Framework -- 2.3.2 Stratigraphic and Tectonic Units -- 2.3.3 Deformation
2.3.4 Dhala Impact Crater -- 2.3.5 Crustal Evolution -- 2.4 Meghalaya Craton -- 2.4.1 Limits of the Craton -- 2.4.2 Geological Framework -- 2.4.3 Tectonics -- 2.5 Bastar Craton (BC) -- 2.5.1 Tectonic Boundaries -- 2.5.2 Major Litho-tectonic Components -- 2.6 Singhbhum Craton -- 2.6.1 Location -- 2.6.2 Geological and Tectonic Framework -- 2.7 Dharwar Craton -- 2.7.1 Introduction -- 2.7.2 Geological and Tectonic Framework -- 2.7.3 Dharwar Greenstone Belts -- 2.7.4 Closepet Granite (Calc-alkaline to Potassic Plutons) -- 2.7.5 Major Shear Zones -- 2.7.6 Proterozoic Mafic Dikes -- 2.7.7 Deformation
2.7.8 Metamorphism -- 2.7.9 Crustal Evolution -- References -- 3 Tectonics of Sri Lanka -- 3.1 Introduction -- 3.2 Geological Framework -- 3.2.1 Highland Complex (HC) -- 3.2.2 Vijayan Complex (VC) -- 3.2.3 Wanni Complex (WC) -- 3.2.4 Kadugannawa Complex (KC) -- 3.3 Deformation -- 3.3.1 Structures of the Highland Complex (HC) -- 3.3.2 Structures of the Vijayan Complex (VC) -- 3.3.3 Structures of the Wanni Complex (WC) -- 3.4 Metamorphism -- 3.5 Geochronology -- 3.6 Sri Lankan Thrusts and Faults -- 3.7 Crustal Evolution -- References -- 4 Proterozoic Mobile Belts -- 4.1 Introduction
4.2 Aravalli-Delhi Mobile Belt (ADMB) -- 4.2.1 Location -- 4.2.2 Regional Geological Setup -- 4.2.3 Aravalli Mobile Belt -- 4.2.4 Delhi Mobile Belt -- 4.2.5 Neoproterozoic Tectonics in the ADMB -- 4.2.6 Orogenies During Aravalli and Delhi -- 4.2.7 The Crustal Evolutionary Models -- 4.3 Central Indian Tectonic Zone (CITZ) -- 4.3.1 Location -- 4.3.2 Distribution -- 4.3.3 Son-Narmada South Fault (SNSF) -- 4.3.4 Gavilgarh-Tan Shear Zone (GTSZ) -- 4.3.5 Central Indian Shear Zone (CIS) -- 4.3.6 Great Indian Proterozoic Fold Belt (GIPFOB) -- 4.3.7 Plate Tectonic Models -- 4.4 Singhbhum Mobile Belt (SMB)
Summary 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
Notes 4.4.1 Location
Bibliography Includes bibliographical references
Notes Print version record
Subject Plate tectonics -- Southeast Asia
Geological surface processes (geomorphology)
Geographical information systems (GIS) & remote sensing.
Geophysics.
Science -- Earth Sciences -- Geology.
Science -- Earth Sciences -- Geography.
Science -- Geophysics.
Plate tectonics
Southeast Asia
Form Electronic book
Author Banerjee, D. M.
Kale, Vivek S
ISBN 9783030428457
3030428451