Original paper
Crustal growth of the Eastern Dharwar Craton: a Neoarchean collisional orogeny?
Volume: 489, Issue: 1, Pages: 51 - 77
Published: Jan 1, 2020
Abstract
The Eastern Dharwar Craton (EDC) is predominantly made of Neoarchean potassic granitoids with subordinate linear greenstone belts. Available geochemical and isotopic systematics of these granitoids suggest variations in the source and petrogenetic mechanisms. By compiling the available geochemical data, these granitoids can be classified into four groups, namely: TTGs (tonalite–trondhjemite–granodiorite); sanukitoids; biotite and two-mica...
Paper Details
Title
Crustal growth of the Eastern Dharwar Craton: a Neoarchean collisional orogeny?
Published Date
Jan 1, 2020
Volume
489
Issue
1
Pages
51 - 77
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Notes
History