Interaction between felsic granitoids and mafic dykes in Bundelkhand Craton: A field, petrographic and crystal size distribution study
Author:
Funder
University Grants Commission
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
http://link.springer.com/article/10.1007/s12040-018-1003-7/fulltext.html
Reference66 articles.
1. Armienti P, Pareschi M T, Innocenti F and Pompilio M 1994 Effects of magma storage and ascent on the kinetics of crystal growth; Contrib. Mineral. Petrol. 115 402–414.
2. Barbarin B 2005 Mafic magmatic enclaves and mafic rocks associated with some granitoids of the central Sierra Nevada batholiths California nature origin and relations with the hosts; Lithos 80 155–177.
3. Barbarin B and Didier J 1991 Review of the main hypothesis proposed for the genesis and evolution of mafic microgranular enclaves; Enclaves and Granite Petrology 13 367–373.
4. Barbarin B and Didier J 1992 Genesis and evolution of mafic microgranular enclaves through various types of interaction between coexisting felsic and mafic magmas; Trans. Roy. Soc. Edinb. Earth Sci. 83 145–153.
5. Basu A K 1986 Geology of Bundelkhand Granite massif Central India; Record, GSI 117(2) 61–124.
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