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:

06 Aug 2015 09:23

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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