Fluid processes in the early Earth and the growth of continents

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...

Full description

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

Internet

http://purl.org/au-research/grants/arc/DP200101104
http://hdl.handle.net/20.500.11937/90818

Similar Items