Hydrothermal Fracture Controlled Vein Type Uranium Mineralization in the Paleoproterozoic Bijawar Group of Rocks, Sonrai Basin, Lalitpur District, U.P. – Fresh Findings from Subsurface Borehole Data

Authors

  • T. P. S. Rawat
     Atomic Minerals Directorate for Exploration and Research, Department of Atomic Energy, West Block 7, R.K. Puram, New Delhi - 110 066
  • Madhuparna Roy
     Atomic Minerals Directorate for Exploration and Research, Department of Atomic Energy, West Block 7, R.K. Puram, New Delhi - 110 066
  • G. B. Joshi
     Atomic Minerals Directorate for Exploration and Research, Department of Atomic Energy, Begumpet, Hyderabad – 500 016

DOI:

https://doi.org/10.1007/s12594-018-0816-y

Abstract

Sonrai basin, located along the southwestern margin of Bundelkhand Granite-Gneiss Complex (BGC) is known for its base metal and phosphorite mineralization. Uranium mineralization of appreciable grade and thickness was reported in Pisnari block in the northern part of this basin during sub-surface exploration activity in 1976-97. This was in the form of uranium-bitumin association within fractures in the carbonate-terrigenous sediments of Gorakalan shale, Rohini carbonate and Bandai sandstone of Sonrai Formation of Bijawar Group. Similar mineralization was also noted within the lower chloritic shale member of Solda Formation of the same Group. During subsequent drilling activity at a later phase (2005-09), uranium rich zones within Rohini carbonate and chloritic shale members were corroborated by the interception of mineralized bands in two boreholes drilled near Pisnari. Petrographic study of radioactive core samples reveal that uranium mineralization is closely associated with globular carbonaceous matter and sulphides along the fractures. Uranium is either adsorbed in carbonaceous matter or occurs as ultrafine inclusions of coffinite within carbonaceous matter. An additional phase of secondary uranium mineral (uranophane) is also noted in one of the boreholes. The uranium minerals, in association with sulphides, fill up moderately dipping fractures (approximately 15° towards North) which are oblique to the core axis of the inclined borehole and thus, the mineralization is characterized as hydrothermal fracture-controlled vein type mineralisation. C-HN- S analysis of carbonaceous matter occurring in close association with the uranium minerals reveal heterogeneity in composition with respect to carbon and sulfur. The present paper aims at discussing the geological, petrological and radiometric aspects of this mineralization, so as to enhance the understanding of the same.

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Issue

Volume 91, Issue 1, January 2018 Pages (1-132)

Section

Research Articles

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Published

2018-01-01

How to Cite

Rawat, T. P. S., Roy, M., & Joshi, G. B. (2018). Hydrothermal Fracture Controlled Vein Type Uranium Mineralization in the Paleoproterozoic Bijawar Group of Rocks, Sonrai Basin, Lalitpur District, U.P. – Fresh Findings from Subsurface Borehole Data. Journal of Geological Society of India, 91(1), 25–31. https://doi.org/10.1007/s12594-018-0816-y
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