The TTG-Amphibolite Terrains of Arctic Fennoscandia : Infinite Networks of Amphibolite Metatexite-Diatexite Transitions
The Earth's early basaltic crust converted episodically into felsic TTG (tonalite-trondhjemite-granodiorite) crust by unknown tectonic processes. To contribute to the debate on the possible tectonic settings of TTGs, this article illustrates and explains migmatite structures of Meso- to Neoarch...
Published in: | Frontiers in Earth Science |
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Main Author: | |
Other Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Frontiers Media
2020
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Subjects: | |
Online Access: | http://hdl.handle.net/10138/318181 |