Abstract
This study aims to present the three mappable lithounits of the Ghaghar Formation of the Kaimur Group, which have been reported for the first time in the eastern part of the Vindhyan basin exposed in Kaimur district, Bihar, India. These litho-units are coarse to medium-grained sandstone (Facies-A), fine to medium-grained sandstone, with intercalated siltstone (Facies-B), and medium to coarse-grained sandstone (Facies-C). Mineralogically and geochemically these units are sub-lithic arenite and arkose in composition. Based on heavy mineral assemblages, presence of rock fragments, and paleocurrent direction, the possible sources are presumed to be the Chhotanagpur Gneissic Complex and the Mahakoshal Group of rocks, which lie towards the south and south-west. The Ghaghar Formation shows low concentrations of Na2O, TiO2, MgO, CaO, Cu, Co, Pb, Th, and Nb with high concentrations of Ba, Cr, Zr, Y, and V. REE plot shows flat LREE and HREE along with the values of (La/Sm)N, (La/Yb)N and (Gd/ Yb)N, and Eu anomaly allows us to deduce that the sediments were mainly sourced from felsic igneous rocks, such as granites. In binary diagrams, all the samples predominantly come in the field of passive margin tectonic setting except a few samples, which fall in the fields of the active continental margin and continental island arc. Besides, the detailed field observations and sedimentological studies were carried out in facies-A and facies-B based on the concept of Sequence Stratigraphy. It is assumed that the facies-A is presumably to be formed in Lowstand System Tract. The combination of two processes Transgressive System Tract and the Highstand System Tract are responsible for the formation of facies-B. Thus, on the above-mentioned observations, it may be indicated that the beach, sub-tidal to inter-tidal environments were responsible for the deposition of these siliciclastic rocks.
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Data availability
The datasets generated during the current study are available from the corresponding author on reasonable request. All the aforesaid mentioned datasets are not publicly available due to the policy of the parent organization i.e. the Geological Survey of India but are available from the corresponding author on reasonable request.
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The authors are honestly obliged to the Director General, Geological Survey of India for according necessary permission to publish this manuscript. They are also thankful to the Deputy Director General, Geological Survey of India, SU: Bihar for cooperation, constant encouragement, guidance, and valuable suggestions during the work. Sincere thanks to Dr. Manish Kumar Yadav of the Geological Survey of India for providing the details of analytical techniques. This paper is the outcome of the Annual Field Season Programme (FSPMIS ID: M1AGS/STM/NC/ER/SU-BR/2017/20848) of the Geological Survey of India, State Unit: Bihar, Patna. The authors are also thankful to the anonymous reviewers and team of the editorial committee for their critical review along with beneficial comments and suggestions provided on a previous version of the manuscript has very much helped in improving the quality of the paper.
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Yadav, P.K., Das, M. & Ray, S. Geology, petrology, and geochemistry of the Mesoproterozoic Kaimur Group of rocks of the Vindhyan Supergroup, Eastern India: implications for depositional environment and sequence stratigraphy. J. Sediment. Environ. 7, 443–469 (2022). https://doi.org/10.1007/s43217-022-00105-7
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DOI: https://doi.org/10.1007/s43217-022-00105-7