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Frontiers | The TTG-Amphibolite Terrains of Arctic Fennoscandia: Infinite Networks of Amphibolite Metatexite-Diatexite Transitions
In the Archaean, the Earth’s early basaltic crust episodically converted into felsic TTG (tonalite-trondhjemite-granodiorite) crust by unknown tectonic proce...
Prolonged parallel chronology of distinct TTG types in the Lake Inari terrain, Arctic Fennoscandia: Implications for a stationary plume-related source
Revealing Archaean crust-formation processes requires understanding of geochemical and chronological differences in granitoids. During the early evolu…
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 pro…
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