Metamorphic rates in collisional orogeny from in situ allanite and monazite dating
The prograde sequence of rare earth minerals recorded in metapelites during regional metamorphism reveals a series of irreversible reactions among silicates and phosphates. In individual samples from the northern Lepontine (Central Alps), allanite is partly replaced by monazite at 560–580 °C. Relic...
| Main Authors: | , , , , , |
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| Format: | Journal Article |
| Published: |
Geological Society of America Inc
2009
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| Online Access: | http://hdl.handle.net/20.500.11937/22329 |