Title: Fission-track ages and uranium concentration in garnets from Rajasthan, India
Abstract: Research Article| May 01, 1976 Fission-track ages and uranium concentration in garnets from Rajasthan, India NAND LAL; NAND LAL 1Department of Physics, Kurukshetra University, Kurukshetra 132119, India Search for other works by this author on: GSW Google Scholar K. K. NAGPAUL; K. K. NAGPAUL 1Department of Physics, Kurukshetra University, Kurukshetra 132119, India Search for other works by this author on: GSW Google Scholar K. K. SHARMA K. K. SHARMA 2Wadia Institute of Himalayan Geology, Delhi University, Delhi 110007, India Search for other works by this author on: GSW Google Scholar Author and Article Information NAND LAL 1Department of Physics, Kurukshetra University, Kurukshetra 132119, India K. K. NAGPAUL 1Department of Physics, Kurukshetra University, Kurukshetra 132119, India K. K. SHARMA 2Wadia Institute of Himalayan Geology, Delhi University, Delhi 110007, India Publisher: Geological Society of America First Online: 01 Jun 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Geological Society of America GSA Bulletin (1976) 87 (5): 687–690. https://doi.org/10.1130/0016-7606(1976)87<687:FAAUCI>2.0.CO;2 Article history First Online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation NAND LAL, K. K. NAGPAUL, K. K. SHARMA; Fission-track ages and uranium concentration in garnets from Rajasthan, India. GSA Bulletin 1976;; 87 (5): 687–690. doi: https://doi.org/10.1130/0016-7606(1976)87<687:FAAUCI>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract Fission-track ages determined from garnets in pegmatite and garnetiferous amphibolite from Bhilwara and Ajmer districts of Rajasthan range from 900 m.y. to 1,370 m.y. They date the time of formation of the pegmatites (about 1,000 m.y. B.P.) and the metamorphism during F1 (∼1,400 m.y. B.P.) folding in the area. The uranium content of the garnets varies from 1.76 × 10−8 g/g to 21.4 × 10−8 g/g. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
Publication Year: 1976
Publication Date: 1976-01-01
Language: en
Type: article
Indexed In: ['crossref']
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Cited By Count: 20
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