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-Reference-Cited by-同舟云学术

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

Published:2014-01 Issue: Volume:79 Page:72-85
ISSN:1367-9120
Container-title:Journal of Asian Earth Sciences
language:en
Short-container-title:Journal of Asian Earth Sciences

Author:

Anand R.,Balakrishnan S.,Kooijman E.,Mezger K.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference99 articles.

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2. Anand, R., Balakrishnan, S., Mezger, K., 2005. Geochemical and Geochronological Studies on Titanites from the Granitoid Rocks of the Eastern Dharwar Craton, South India. Geophysical Research Abstracts 7, SRef-ID: 1607-7962/gra/EGU05-A-01565.

3. Pb and Nd isotope constraints on the origin of high Mg and tholeiitic amphibolites, Kolar schist belt, south India;Balakrishnan;Contributions to Mineralogy and Petrology,1990

4. U–Pb ages for zircon and titanite from the Ramagiri area, southern India: evidence for accretionary origin of the eastern Dharwar Craton during the late Archean;Balakrishnan;Journal of Geology,1999

5. Basir, S.R., 2000. Geochemistry and Petrogenesis of Granitic Rocks around Hutti Schist Belt, Dharwar Craton. Unpub. Ph.D. Thesis, IIT-Roorkee, Roorkee. 119p.

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