Journal of Geological Society of India (Online archive from Vol 1 to Vol 78)

H. K. Sabot ¹, A. V. Subrahmanyam ², S. Nayak ²

Affiliations
1 AMD Complex, Hyderabad - 500 016, IN
2 AMD ER/DAE, Hyderabad - 500 016, IN

Abstract

No Abstract.

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H. K. Sabot ¹, Omprakash S. Sarate

Affiliations
1 AMD Hyderabad - 500 016, IN

Abstract

No Abstract.

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G. S. Yadav ¹, Rakesh Mohan ², H. K. Sabot ³, M. Nagendra Kumar ², S. Q. Hoda ²

Affiliations
1 Atomic Minerals Directorate for Exploration and Research, Department of Atomic Energy, Jaipur - 302 030, IN
2 Atomic Minerals Directorate for Exploration and Research, Department of Atomic Energy, Shillong - 793 011, IN
3 Atomic Minerals Directorate for Exploration and Research, Department of Atomic Energy, Hyderabad - 500 016, IN

Abstract

Significant Sandstone-Type uranium mineralisation is recorded from the Rongcheng Plateau and Rongdi nala, located north and WNW of Balphakram Plateau, South Garo Hills district, Meghalaya. Mineralisation is associated with grey coloured, medium to coarse grained, poorly sorted arkosic Wacke-Subarkose suite of sandstones, belonging to the late Cretaceous Mahadek Formation. Sixteen uranium occurrences located 2-30 m above crystalline basement and with dimensions varying from 5 to 300 m × 0.5 to 4 m, have been identified. Grab samples have assayed up to 0.52% eU₃O₈ 0.46%U₃O₈ (beta/gamma) and <0.010%Tho₃. The fertile Precambrian basement crystallines constitute the source of uranium. Presence of organic matter and pyrite in the sandstone provided reducing environment for deposition of pitchblende as the principal discrete uranium mineral.

Keywords

U-mineralisaton, Sandstone-Type, Mahadek Formation, Uraninite, Balphakram Area, Meghalaya.

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