On the origin of Archaean TTGs by migmatization of mantle plume-related metabasalts : Insights from the Lake Inari terrain, Arctic Fennoscandia

The conversion of basaltic crust into a thick, buoyant felsic crust of tonalite-trondhjemite-granodiorite (TTG) composition has been a fundamental process in the Earth's evolution during the Archaean Eon (4.03–2.50 Ga). The proposition that TTGs have formed as a result of the partial melting of...

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Bibliographic Details
Main Authors: Halla, Jaana, Joshi, Kumar Batuk, Luttinen, Arto, Heilimo, Esa, Kurhila, Matti
Other Authors: Finnish Museum of Natural History
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier B.V. 2024
Subjects:
Online Access:http://hdl.handle.net/10138/577485