| Reference Type | Journal (article/letter/editorial) |
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| Title | Petrography and Geochemistry of the Radioactive Albitites and their Genesis: Maonda Area, North Rajasthan |
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| Journal | Journal Geological Society of India |
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| Authors | Jain, Rajan B. | Author |
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| Yadav, O. P. | Author |
| Rahman, M. | Author |
| Thippeswamy, S. | Author |
| Fahmi, S. | Author |
| Sharma, D. K. | Author |
| Singh, Govind | Author |
| Year | 1999 (April 1) | Volume | 53 |
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| Page(s) | 407-415 | Issue | 4 |
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| Publisher | Geological Society of India | Place | Bangaluru, India |
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| URL | |
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| DOI | doi:10.17491/jgsi/1999/530403Search in ResearchGate |
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| Generate Citation Formats |
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| Classification | Not set | LoC | Not set |
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| Mindat Ref. ID | 19366286 | Long-form Identifier | mindat:1:5:19366286:7 |
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| GUID | 0 |
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| Full Reference | Jain, Rajan B.; Yadav, O. P.; Rahman, M.; Thippeswamy, S.; Fahmi, S.; Sharma, D. K.; Singh, Govind (1999) Petrography and Geochemistry of the Radioactive Albitites and their Genesis: Maonda Area, North Rajasthan. Journal Geological Society of India, 53 (4). 407-415 doi:10.17491/jgsi/1999/530403 |
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| Plain Text | Jain, Rajan B.; Yadav, O. P.; Rahman, M.; Thippeswamy, S.; Fahmi, S.; Sharma, D. K.; Singh, Govind (1999) Petrography and Geochemistry of the Radioactive Albitites and their Genesis: Maonda Area, North Rajasthan. Journal Geological Society of India, 53 (4). 407-415 doi:10.17491/jgsi/1999/530403 |
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| In | (1999, April) Journal of the Geological Society of India Vol. 53 (4). Geological Society of India |
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| Abstract/Notes | Abstract
A partly concealed radioactive alibitized pegmatoid/quartz albitite body (1200 m x 0.5 to 20 m) containing 0.010 to 0.190% U3O8 and 0.007 to 0.076% ThO2 and about 20 brick red coloured albitite lenses varying in dimension from 13 m x 7 m to 220 m x 12-30 m and containing 0.022 to 3.50% U3O8 and 2 are described at Banjaron Ki Dhani, new Maonda in north Rajasthan. Davidite, brannerite, rutile, anatase, zircon, monazite and traces of uraninite have been identified in the albitites. A metasomatic origin for the albitites is suggested. The distribution of albitites along NE-SW to NW-SE and E-W trending weak structural planes and the coincidence of 'Albitite Line' with Kaliguman lineament, demonstrates the tectonic control of albitization. |
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