Petrogenesis of mafic dykes from the western Bastar craton of Central India and their relation to outgrowth of Columbia supercontinent
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/s00710-020-00695-y.pdf
Reference131 articles.
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2. Alam M, Naushad M, Wanjari N, Ahmad T (2009) Geochemical characterizations of mafic magmatic rocks of the central Indian shield: implication for Precambrian crustal evolution. J Virtual Explor. https://doi.org/10.3809/jvirtex.2009.00246
3. Baer G, Heimann A (1995) Physics and chemistry of dykes. Balkema, Rotterdam
4. Bhowmik SK, Wilde SA, Bhandari A (2011) Zircon U-Pb/Lu-Hf and monazite chemical dating of the Tirodi biotite gneiss: implication for latest Palaeoproterozoic to early Mesoproterozoic orogenesis in the central Indian tectonic zone. Geol J 46:574–596
5. Bleeker W (2003) The late Archaean record: a puzzle in ca. 35 pieces. Lithos 71:99–134
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