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...
| Main Authors: | , , |
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| Format: | Journal Article |
| Published: |
Mineralogical Society of America and several other scientific societies
2011
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| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/47594 |