Organizing melt flow through the crust

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Organizing melt flow through the crust

Melt that crystallizes as granite at shallow crustal levels in orogenic belts originates from migmatite and residual granulite in the deep crust; this is the most important mass-transfer process affecting the continents. Initially melt collects in grain boundaries before migrating along structural f...

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Bibliographic Details
Main Authors:	Brown, M., Korhonen, Fawna, Siddoway, C.
Format:	Journal Article
Published:	Mineralogical Society of America and several other scientific societies 2011
Subjects:	migmatite dike granulite ductile fracturing melt flow granite
Online Access:	http://hdl.handle.net/20.500.11937/47594

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