If cordierite is treated as an anhydrous mineral, the composition of garnet and cordierire, coexisting with quartz and silliminate, depends on total pressure and temperature. Phase relations may be deduced by combining some available experimental work with several approximations. Assuming ideal ioni
β¦ LIBER β¦
Cordierite as an indicator of thermodynamic conditions of petrogenesis
β Scribed by Viktor A. Kurepin
- Book ID
- 106088447
- Publisher
- Springer
- Year
- 2010
- Tongue
- English
- Weight
- 731 KB
- Volume
- 160
- Category
- Article
- ISSN
- 0010-7999
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