Phase Relations in Peridotitic and Pyroxenitic Rocks in the Model Systems CMASH and NCMASH
Alpine-type peridotites and associated pyroxenites are found as lenses in the continental crust in many different orogens. The reconstruction of the pressure–temperature (<rm>P</rm>–<rm>T</rm>) evolution of these rocks is, however, difficult or even impossible. With geothermo...
| Published in: | Journal of Petrology |
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| Main Author: | |
| Format: | Text |
| Language: | English |
| Published: |
Oxford University Press
2000
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| Subjects: | |
| Online Access: | http://petrology.oxfordjournals.org/cgi/content/short/41/1/69 https://doi.org/10.1093/petrology/41.1.69 |