Coupled Assimilation and Fractional Crystallization (AFC) and Mantle Plume Source(s) Contribution in the Generation of Paleoproterozoic Mafic Dykes of the Eastern Dharwar Craton, Southern India-Reference-Cited by-同舟云学术

Coupled Assimilation and Fractional Crystallization (AFC) and Mantle Plume Source(s) Contribution in the Generation of Paleoproterozoic Mafic Dykes of the Eastern Dharwar Craton, Southern India

Published:2019-02 Issue:2 Volume:93 Page:157-162
ISSN:0016-7622
Container-title:Journal of the Geological Society of India
language:en
Short-container-title:J Geol Soc India

Author:

Pandey Ashutosh,Chalapathi Rao N. V.

Publisher

Springer Science and Business Media LLC

Subject

Geology

Link

http://link.springer.com/article/10.1007/s12594-019-1144-6/fulltext.html

Reference51 articles.

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3. Biggar, G.M. (1983) Crystallization of plagioclase, augite, and olivine in synthetic systems and in tholeiites. Min. Mag., v.47, pp.161–176.

4. Cadman, A.C., Tarney, J. and Baragar, W.R.A. (1995) Nature of mantle source contributions and the role of contamination and in situ crystallization in the petrogenesis of Proterozoic mafic dykes and flood basalts Labrador. Contrib. Mineral. Petrol., v.122, pp.213–229.

5. Chadwick, B., Vasudev, V.N. and Hegde, G.V. (2000) The Dharwar craton, southern India, interpreted as the result of Late Archean oblique convergence. Precambrian Res., v.99, pp.91–111.

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