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2018 | OriginalPaper | Buchkapitel

Paleogene Tectonic and Sedimentation History of the Andaman-Nicobar Accretionary Arc, Northeast Indian Ocean

verfasst von : P. C. Bandopadhyay, Andrew Carter

Erschienen in: The Indian Paleogene

Verlag: Springer International Publishing

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Abstract

The Andaman-Nicobar archipelago in the northeastern Indian Ocean is a nonvolcanic outer arc island chain developed by tectonic accretion of sediments and ocean crust along the eastern margin of the subducting Indian lithosphere. The Paleogene stratigraphy of the island chain comprises olistostromes, olistoliths and coarse-grained volcaniclastic turbidite facies, and reefal limestones of late Paleocene-Eocene Mithakhari Melange and finer-grained siliciclastic turbidites (Andaman Flysch) of Oligocene age. The lower Paleogene sedimentary rocks were deposited in shallow-water basins formed on the upper trench slope and growing accretionary wedge and contain material sourced from a local volcanic arc and eroded ophiolite. By contrast, the Oligocene continent-derived siliciclastic sediments were originally deposited outside of the accretionary wedge as part of a large submarine fan system. Subsequent deformation and thrusting juxtaposed these different formations as trench rollback progressed and the accretionary wedge expanded westwards.

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Vorheriges Kapitel Paleogene Stratigraphy of India: An Overview

Nächstes Kapitel Geotectonic Evolution of the Paleogene Basins in and Around Peninsular India as Revealed in Seismic Sections and Deep Drilling

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Titel: Paleogene Tectonic and Sedimentation History of the Andaman-Nicobar Accretionary Arc, Northeast Indian Ocean
verfasst von: P. C. Bandopadhyay
Andrew Carter
Verlag: Springer International Publishing
Buch: The Indian Paleogene
Print ISBN: 978-3-319-77442-8

Electronic ISBN: 978-3-319-77443-5

Copyright-Jahr: 2018
DOI: https://doi.org/10.1007/978-3-319-77443-5_2