Petrographic Study of the Meso-Neo Proterozoic Kaimur Sandstone, Vindhyan Supergroup, Chittorgarh, southeastern Rajasthan, India: Implication for Provenance, Tectonic Setting and Paleoclimate

Authors

  • Mujeebul Hasan Author

Keywords:

Kaimur Sandstone, Petrography, X-ray diffraction, Provenance, Tectonic setting, Southeastern Rajasthan.

Abstract

Proterozoic Kaimur Sandstone succession rests unconformably on calcium carbonate-rich succession of the Khorip Group (Lower Vindhyan) in and around Chittorgarh, southeastern part of Rajasthan. The Kaimur Group consists multicoloured, medium -to fine-grained, thick beds of sandstones with thin beds of sandy shale and flagstone, display of various primary sedimentary structures such as current bedding, ripple marks and mud cracks. Kaimur quartz arenite composed of varieties of quartz with rare feldspar, mica, rock fragments, and heavy minerals. The X-ray diffraction (XRD) data has shown that quartz is more abundant with little iron oxide mineral. The provenance, tectonic setting and paleoclimatic of the Kaimur Sandstone is evaluated using integrated petrographic studies. Analysis reveals detrital derivation from granitic and metamorphic Precambrian basement source rocks of a craton interior setting with a minor quartzose recycled sedimentary rock. Intense weathering in warm and humid climate indicated lack of feldspar and rock fragments. Paleocurrent indicate flow from NW and SW.

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Published

2019-12-31

How to Cite

Hasan, M. (2019). Petrographic Study of the Meso-Neo Proterozoic Kaimur Sandstone, Vindhyan Supergroup, Chittorgarh, southeastern Rajasthan, India: Implication for Provenance, Tectonic Setting and Paleoclimate. Journal of The Indian Association of Sedimentologists (peer Reviewed), 36(1), 51–64. Retrieved from http://journal.indiansedimentologists.com/ojs/index.php/1/article/view/78
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