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Phase equilibria constraints on Archean crustal genesis from crystallization experiments on trondhjemite with water at 10-17 kbar

Year: 1990
Type: book-chapter
Abstract: The formation of continental crust during the Archean and early Proterozoic occurred through \na different mechanisms than the currently active processes of calc-alkaline volcanism in orogenic \nregions. In view that most crustal growth models imply that by the end of the Archean a continental \nmass equivalent to 75% or more of the current crust had evolved, it seems highly relevant to study \nearly crustal genesis.
Language: English
Open Access status: green
OpenAlex ID: W317871709
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