Fluid processes in the early Earth and the growth of continents

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Fluid processes in the early Earth and the growth of continents

Water is an essential ingredient in transforming primitive mantle-derived (mafic) rocks into buoyant (felsic) continental crust, thereby driving the irreversible differentiation of Earth's lithosphere. The occurrence in Archaean cratons of sodic granites of the tonalite–trondhjemite–granodiorit...

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Bibliographic Details
Main Authors:	Hartnady, Michael, Johnson, Tim, Schorn, S., Hugh Smithies, R., Kirkland, Christopher, Richardson, S.H.
Format:	Journal Article
Language:	English
Published:	ELSEVIER 2022
Subjects:	Science & Technology Physical Sciences Geochemistry & Geophysics fluid processes komatiite tonalite-trondhjemite-granodiorite (TTG) Archaean crustal evolution ISUA SUPRACRUSTAL BELT OXYGEN ISOTOPES ARCHEAN CRUST ORIGIN SUBDUCTION ROCKS PETROGENESIS METAMORPHISM AMPHIBOLITE GENERATION
Online Access:	http://purl.org/au-research/grants/arc/DP200101104 http://hdl.handle.net/20.500.11937/90818

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