Palaeo-tectonic environment of the Precambrian basaltic mafic dykes on the application of chemical discriminants

Details Palaeo-tectonic environment of the Precambrian basaltic mafic dykes on the application of chemical discriminants Palaeo-tectonic environment of the Precambrian basaltic mafic dykes on the application of chemical discriminants

Nov 1986

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1986ineps..95..351r&link_type=abstract

Proceedings of the Indian Academy of Sciences - Earth and Planetary Sciences, Volume 95, Issue 3, pp.351-361

Computer Science

Palaeo-Tectonic Environment, Mafic Dykes, Chemical Discriminant

Scientific paper

Dykes of Chitaldurg and Newer Dolerite I are OFB and represent early attempts to rift and to generate oceanic crust. Shimoga dykes are CAB and belong to orogenic phase. Guntur dykes and Ananthapur-Chittoor dykes are OIB and these are related to ‘hot spot’. Newer Dolerite II is CONB and belongs to healing and filling of fractured crust. The Cuddapah dykes are transitional to all magma types and these represent a compound event of rifting and filling of fractured continental crust.

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