Published March 1990
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Phase equilibria constraints on Archean crustal genesis from crystallization experiments on trondhjemite with water at 10-17 kbar
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Abstract
The formation of continental crust during the Archean and early Proterozoic occurred through a different mechanisms than the currently active processes of calc-alkaline volcanism in orogenic regions. In view that most crustal growth models imply that by the end of the Archean a continental mass equivalent to 75% or more of the current crust had evolved, it seems highly relevant to study early crustal genesis.
Additional Information
© 1990 Lunar and Planetary Institute.Attached Files
Published - Wyllie_1990p1268.pdf
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- CaltechAUTHORS:20160414-123058047
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