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Kundu, Abhik
- A Note on Seismic Evidences during the Sedimentation of Panchet formation, Damodar Basin, Eastern India: Banspetali Nullah Revisited
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Authors
Abhik Kundu
1,
Bapi Goswami
2
Affiliations
1 Asutosh College, 92 S P Mukherjee Road, Kolkata-700026, IN
2 J K College, Purulia-723101, IN
1 Asutosh College, 92 S P Mukherjee Road, Kolkata-700026, IN
2 J K College, Purulia-723101, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 72, No 3 (2008), Pagination: 400-404Abstract
The Damodar basin of eastern India preserves both Lower and Upper Gondwana sediments. It was thought earlier that deposition of Panchet Formation ot Upper Gondwana took place in a tectonitally undisturbed condition. However present study reveals that some beds of Panchet Formation were seismically disturbed as they contain several horizons of soft sediment deformation structures like deformed cross beds, convolute laminae, mud dykes flame structures, pseudonodules chaotic bedding and drifted sediment blocks. The preservation of these penecontemporaneous deformation structures clearly suggests that earthquakes were responsible for the deformation and warrants further study on the tectonic history of the basin.Keywords
Panchet Formation, Seismites, Soft Sediment, Deformation Structures, Damodar Basin.
- Sedimentary Facies and Soft-Sediment Deformation Structures in the Late Miocene-Pliocene Middle Siwalik Subgroup, Eastern Himalaya, Darjiling District, India
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Authors
Affiliations
1 Department of Geology, Asutosh College, 92, S. P. Mukherjee Road, Kolkata-700 026, IN
2 Department of Geology, University of Calcutta, 35, Ballygunj Circular Road, Kolkata-700 029, IN
3 Department of Earth Sciences, Indian Institute of Technology, Powai, Mumbai - 400 076, IN
4 Department of Geology, University of Pretoria, Pretoria 0002, ZA
1 Department of Geology, Asutosh College, 92, S. P. Mukherjee Road, Kolkata-700 026, IN
2 Department of Geology, University of Calcutta, 35, Ballygunj Circular Road, Kolkata-700 029, IN
3 Department of Earth Sciences, Indian Institute of Technology, Powai, Mumbai - 400 076, IN
4 Department of Geology, University of Pretoria, Pretoria 0002, ZA
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 78, No 4 (2011), Pagination: 321-336Abstract
The Himalayan fold-and-thrust belt has propagated from its Tibetan hinterland to the southern foreland since ∼55 Ma. The Siwalik sediments (∼20 - 2 Ma) were deposited in the frontal Himalayan foreland basin and subsequently became part of the thrust belt since ∼12 Ma. Restoration of the deformed section of the Middle Siwalik sequence reveals that the sequence is ∼325 m thick. Sedimentary facies analysis of the Middle Siwalik rocks points to the deposition of the Middle Siwalik sediments in an alluvial fan setup that was affected by uplift and foreland-ward propagation of Greater and Lesser Himalayan thrusts. Soft-sediment deformation structures preserved in the Middle Siwalik sequence in the Darjiling Himalaya are interpreted to have formed by sediment liquefaction resulting from increased pore-water pressure probably due to strong seismic shaking. Soft-sediment structures such as convolute lamination, flame structures, and various kinds of deformed cross-stratification are thus recognized as palaeoseismic in origin. This is the first report of seismites from the Siwalik succession of Darjiling Himalaya which indicates just like other sectors of Siwalik foreland basin and the present-day Gangetic foreland basin that the Siwalik sediments of this sector responded to seismicity.Keywords
Soft-Sediment Deformation, Seismite, Siwalik, Neogene, Foreland Basin, Siwalik Sedimentary Facies.References
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