Taking the temperature of Earth’s hottest crust
The limitations of conventional thermobarometry and petrogenetic grids for determining the peak P–T conditions of granulites are well known. These limitations have been overcome during the past decade with the calibration of single mineral thermometers, particularly Al-in-orthopyroxene, Zr-in-rutile...
| Main Authors: | , , , |
|---|---|
| Format: | Journal Article |
| Published: |
Elsevier Science BV
2014
|
| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/31162 |