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Yadav, G. S.
- Recognition of a New Albitite Zone in Northern Rajasthan:Its Implications on Uranium Mineralization
Abstract Views :160 |
PDF Views:52
Authors
Affiliations
1 Jamshedpur 831 002, IN
2 Center for Remote Sensing, Bharthidasan University, Tiruchirappalli 620 023, IN
3 Thiruvananthpuram 659 012, IN
4 Hyderabad 500 016, IN
1 Jamshedpur 831 002, IN
2 Center for Remote Sensing, Bharthidasan University, Tiruchirappalli 620 023, IN
3 Thiruvananthpuram 659 012, IN
4 Hyderabad 500 016, IN
Source
Current Science, Vol 108, No 11 (2015), Pagination: 1994-1998Abstract
No Abstract.- U-Pb, Pb-Pb and Sm-Nd Ages of Davidite within Albitite Zone from Bichun, Jaipur District, Rajasthan, India:Possible Link between Uranium Mineralization and Grenvillian Orogeny
Abstract Views :123 |
PDF Views:26
Authors
G. S. Yadav
1,
U. K. Pandey
2,
S. L. Aravind
3,
P. K. Panchal
3,
A. S. Venkatesh
4,
P. R. Sahoo
4,
A. K. Chaturvedi
2,
A. K. Rai
2,
P. S. Parihar
2
Affiliations
1 Atomic Minerals Directorate for Exploration and Research, Jamshedpur 831 002, IN
2 Atomic Minerals Directorate for Exploration and Research, Hyderabad 500 016, IN
3 Atomic Minerals Directorate for Exploration and Research, Jaipur 302 030, IN
4 Department of Applied Geology, Indian Institute of Technology (Indian School of Mines), Dhanbad 826 004, IN
1 Atomic Minerals Directorate for Exploration and Research, Jamshedpur 831 002, IN
2 Atomic Minerals Directorate for Exploration and Research, Hyderabad 500 016, IN
3 Atomic Minerals Directorate for Exploration and Research, Jaipur 302 030, IN
4 Department of Applied Geology, Indian Institute of Technology (Indian School of Mines), Dhanbad 826 004, IN
Source
Current Science, Vol 111, No 5 (2016), Pagination: 907-913Abstract
Uranium mineralization in Bichun area, Jaipur district, Rajasthan, India is hosted by albitites within the Banded Gneissic Complex (BGC). Detailed mineralogical and EPMA studies reveal the presence of davidite along with brannerite and uraninite. The U-Pb concordia upper intercept age of 933 ± 13 Ma and Pb-Pb isochron age of 930 ± 4 Ma, on pure davidite fractions indicate the timing of uranium mineralizing event to be ca. 930 Ma. The timing of uranium mineralization can be correlated with the Grenvillian orogeny (ca. 1000 Ma). The Sm-Nd model age (TDM) of daviditeis varies from 1851 to 2200 Ma with εNdi(930 Ma) ranging from -10.7 to -15.5 which shows that the Palaeoproterozoic rocks with crustal component (either within BGC or basement granite) are the source for uranium.Keywords
Albitite Zone, Davidite, Geochronology, Orogeny, Uranium Mineralization.- Gold and Uranium Occurrences in Quartz-Pebble Conglomerate of Iron Ore Group, Bagiyabahal-Baratangra Area, Sundargarh District, Odisha, India
Abstract Views :156 |
PDF Views:17
Authors
Affiliations
1 Atomic Minerals Directorate for Exploration and Research, Jamshedpur 831 002, IN
1 Atomic Minerals Directorate for Exploration and Research, Jamshedpur 831 002, IN