Seismic and non-seismic soft-sediment deformation structures in the Proterozoic Bhander Limestone, central India

Seismic and non-seismic soft-sediment deformation structures in the Proterozoic Bhander Limestone, central India

Numerous soft-sediment deformation structures occur within the Proterozoic Bhander Limestone of an intracratonic sag basin in a 750 m long section along the Thomas River, near Maihar, central India. Part of these deformation structures have most probably a non-seismic origin, but other structures ar...

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Bibliographic Details
Main Authors: Sarkar Subir, Choudhuri Adrita, Banerjee Santanu, Van Loon A.J. (Tom), Bose Pradip K
Format: Article
Language:English
Published: Sciendo 2014-07-01
Series:Geologos
Subjects:
seismites
soft-sediment deformation structures
basin subsidence
bhander limestone
proterozoic
india
Online Access:https://doi.org/10.2478/logos-2014-0008

Internet

https://doi.org/10.2478/logos-2014-0008

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