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Antiquity of the Oceans and Continents

Nutman, Allen


Tracing the origin of the oceans and the division of the crust into distinct oceanic and continental realms relies on incomplete information from tiny vestiges of surviving oldest crust (>3.6 billions years old). Billions of years of tectonism, melting and erosion have obliterated the rest of that crust. Oceans and continental crust already existed almost four billion years ago because water-laid sedimentary rocks of this age have been found and because tonalites dominate in gneissic sequences...[Show more]

CollectionsANU Research Publications
Date published: 2006
Type: Journal article
Source: Elements
DOI: 10.2113/gselements.2.4.223


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