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