The replacement of plagioclase feldspars by albite: Observations from hydrothermal experiments
Oligoclase and labradorite crystals have been experimentally replaced by albite in an aqueous sodium silicate solution at 600°C and 2 kbars. The replacement is pseudomorphic and is characterised by a sharp chemical interface which progresses through the feldspar while preserving the crystallographic...
| Main Authors: | , , , , |
|---|---|
| Format: | Journal Article |
| Published: |
Springer
2010
|
| Online Access: | http://hdl.handle.net/20.500.11937/37309 |