Neoarchean crustal growth by accretionary processes: Evidence from combined zircon–titanite U–Pb isotope studies on granitoid rocks around the Hutti greenstone belt, eastern Dharwar Craton, India.

Anand, R; Balakrishnan, S; Kooijman, E; Mezger, Klaus (2014). Neoarchean crustal growth by accretionary processes: Evidence from combined zircon–titanite U–Pb isotope studies on granitoid rocks around the Hutti greenstone belt, eastern Dharwar Craton, India. Journal of Asian earth sciences, 79, pp. 72-85. Elsevier 10.1016/j.jseaes.2013.09.017

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Item Type:	Journal Article (Original Article)
Division/Institute:	08 Faculty of Science > Institute of Geological Sciences 08 Faculty of Science > Institute of Geological Sciences > Isotope Geology
UniBE Contributor:	Mezger, Klaus
Subjects:	500 Science > 550 Earth sciences & geology
ISSN:	1367-9120
Publisher:	Elsevier
Language:	English
Submitter:	Klaus Mezger
Date Deposited:	27 Apr 2014 16:00
Last Modified:	05 Dec 2022 14:31
Publisher DOI:	10.1016/j.jseaes.2013.09.017
BORIS DOI:	10.7892/boris.46186
URI:	https://boris.unibe.ch/id/eprint/46186

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Neoarchean crustal growth by accretionary processes: Evidence from combined zircon–titanite U–Pb isotope studies on granitoid rocks around the Hutti greenstone belt, eastern Dharwar Craton, India.

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