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...
Main Authors: | , , , , |
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Other Authors: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Elsevier B.V.
2024
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Subjects: | |
Online Access: | http://hdl.handle.net/10138/577485 |