Origin of clinopyroxene megacrysts from the 1.1 Ga Chigicherla-4 kimberlite (CC4), Dharwar craton, southern India: Implications for multi-stage metasomatism of the sub-continental lithospheric mantle

Author:

Babu E.V.S.S.K.ORCID,Dash Sarbajit,Santhosh G.H.N.V.,Mukherjee Abhijeet

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference138 articles.

1. Polymineralic inclusions in kimberlite-hosted megacrysts: implications for kimberlite melt evolution;Abersteiner;Lithos,2019

2. Trace element partitioning between mica-and amphibole-bearing garnet lherzolite and hydrous basanitic melt: 1. Experimental results and the investigation of controls on partitioning behaviour;Adam;Contrib. Miner. Petrol.,2006

3. Agashev, A.M., Pokhilenko, N.P., Takazawa, E., Watanabe, T., Mcdonald, J.A., Sobolev, N.V., Vavilov, M.A., Fomin, A.S., 2001. Do superchondritic Nb / Ta ratios in kimberlites tell the lower mantle plume signature? In: 2nd International Superplume Workshop 3–7.

4. Olivine, and the origin of kimberlite;Arndt;J. Petrol.,2010

5. The Sytykanskaya kimberlite pipe: evidence from deep-seated xenoliths and xenocrysts for the evolution of the mantle beneath Alakit, Yakutia, Russia;Ashchepkov;Geosci. Front.,2015

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