Sequence Stratigraphic Model of Middle Permian Barakar Formation from a Marginal Gondwana Basin, India

Joyjit Dey; Souvik Sen

doi:10.1007/s12583-018-0791-7

Volume 29 Issue 4

Jul 2018

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Journal of Earth Science > 2018 > 29(4): 745-754.

Joyjit Dey, Souvik Sen. Sequence Stratigraphic Model of Middle Permian Barakar Formation from a Marginal Gondwana Basin, India. Journal of Earth Science, 2018, 29(4): 745-754. doi: 10.1007/s12583-018-0791-7

Citation:

Joyjit Dey, Souvik Sen. Sequence Stratigraphic Model of Middle Permian Barakar Formation from a Marginal Gondwana Basin, India. Journal of Earth Science, 2018, 29(4): 745-754. doi: 10.1007/s12583-018-0791-7

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Sequence Stratigraphic Model of Middle Permian Barakar Formation from a Marginal Gondwana Basin, India

doi: 10.1007/s12583-018-0791-7

Joyjit Dey¹,
Souvik Sen^{2
,
,}

1.
Coal India Limited, Central Mine Planning and Design Institute(CMPDI), Regional Institute-3, Jharkhand 829 103, India
2.
Geologix Limited, Dynasty Building, Level-4, Wing-A, Andheri Kurla Road, Andheri(E), Mumbai 400 059, India

More Information

Corresponding author: Souvik Sen
Received Date: 24 Mar 2018
Accepted Date: 12 Apr 2018
Publish Date: 01 Aug 2018

Abstract

Abstract

Gondwana deposits are extensively found across the continents. Here we study the Middle Permian Barakar Formation from the marginal Gondwana Basin, eastern India, being deposited in a normal fault setting. Availability of extensive cores as well as geophysical log suites (gamma-resistivity-density from drilled wells) from the study area helped us achieving high resolution interpretation. Core study identifies fluvial sedimentary architectures, which were correlated with the geophysical logs and modeled field-wide to understand vertical and horizontal facies disposition. The facies analysis has been used to establish a sequence stratigraphic model of the cyclic Barakar deposition. Four major fining upward depositional sequences were identified, each sequence comprises of low accommodation system tract (LAST) at base and high accommodation system tract (HAST) at top. LAST is characterized by vertically stacked, multistory amalgamated channel sandstone dominated facies, while floodplain dominated facies characterizes HAST, reflecting a gradual shift from braided to meandering depositional system from bottom to top of each cycle. Study reveals depocenter to be in the western part, supported by eastward thinning of sediment packets, all being deposited in a half-graben setting.
- fluvial sequence stratigraphy,
- Gondwana sediment,
- Middle Permian,
- Barakar For-mation

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References(41)

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