High-grade metamorphism and partial melting in Archean composite grey gneiss complexes
Much of the exposed Archean crust is composed of composite gneiss which includes a large proportion of intermediate to tonalitic material. These gneiss terranes were typically metamorphosed to amphibolite to granulite facies conditions, with evidence for substantial partial melting at higher grade....
Main Authors: | , , |
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Format: | Journal article |
Language: | English |
Published: |
Wiley
2016
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