The complex hydrothermal history of granitic rocks: Multiple feldspar replacement reactions under subsolidus conditions
Recurring subsolidus re-equilibration of granitic feldspars induced by fluid infiltration events provides a record of fluid-rock interactions that affect large volumes of the Earth's continental crust. This has a direct bearing on the interpretation of the present-day granitic rock mineralogy a...
| Main Authors: | , |
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| Format: | Journal Article |
| Published: |
Oxford University Press
2009
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| Online Access: | http://hdl.handle.net/20.500.11937/31418 |
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