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A Note on the Uranium Mineralisation along Jamual-markundi Fault, Sonbhadra and Sidhi Districts, Uttar Pradesh and Madhya Pradesh


Affiliations
1 Atomic Minerals Directorate for Exploration and Research, New Delhi-110066, India
2 Atomic Minerals Directorate for Exploration and Research, Jaipur -302030, India
3 Atomic Minerals Directorate for Exploration and Research, 313/4, Sector-56, Rail Vihar, Gurgaon, Haryana, India
     

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Surface indications of uranium mineralisation associated with ferruginised brecciated rocks is traceable, intermittently, over a strike length of 25 km, exposed along the Jamual -Markundi Fault (JMF), at the tectonic contact of Neo- to Meso-Proterozoic Vindhyan Supergroup and Paleo-Proterozoic Mahakoshal Group between Gurdah and Mohariya, Sonbhadra and Sidhi districts of U.P. and M.P. respectively. Preliminary investigations reveal uranium (U3Og) content upto 610 ppm with little or no ThO2. Uranium occurs in adsorbed state in the ferruginised groundmass of brecciated rock and probably related to hydrothermal activity. This is the first reported uranium occurrence from this unconformity related geological set up in the Son valley.

Keywords

Uranium mineralisation, Unconformity, Jamual-Markundi fault, Son-valley, U.P., M.P.
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  • A Note on the Uranium Mineralisation along Jamual-markundi Fault, Sonbhadra and Sidhi Districts, Uttar Pradesh and Madhya Pradesh

Abstract Views: 189  |  PDF Views: 2

Authors

D. Bhattacharya
Atomic Minerals Directorate for Exploration and Research, New Delhi-110066, India
G. B. Joshi
Atomic Minerals Directorate for Exploration and Research, New Delhi-110066, India
G. S. Sharma
Atomic Minerals Directorate for Exploration and Research, Jaipur -302030, India
D. B. Sen
Atomic Minerals Directorate for Exploration and Research, 313/4, Sector-56, Rail Vihar, Gurgaon, Haryana, India

Abstract


Surface indications of uranium mineralisation associated with ferruginised brecciated rocks is traceable, intermittently, over a strike length of 25 km, exposed along the Jamual -Markundi Fault (JMF), at the tectonic contact of Neo- to Meso-Proterozoic Vindhyan Supergroup and Paleo-Proterozoic Mahakoshal Group between Gurdah and Mohariya, Sonbhadra and Sidhi districts of U.P. and M.P. respectively. Preliminary investigations reveal uranium (U3Og) content upto 610 ppm with little or no ThO2. Uranium occurs in adsorbed state in the ferruginised groundmass of brecciated rock and probably related to hydrothermal activity. This is the first reported uranium occurrence from this unconformity related geological set up in the Son valley.

Keywords


Uranium mineralisation, Unconformity, Jamual-Markundi fault, Son-valley, U.P., M.P.