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Spinel–garnet lherzolite transition in the system CaO-MgO-Al2O3-SiO2 revisited: an in situ X-ray study

✍ Scribed by M. Walter; T. Katsura; A. Kubo; T. Shinmei; O. Nishikawa; E. Ito; C. Lesher; K. Funakoshi

Book ID
117117064
Publisher
Elsevier Science
Year
2002
Tongue
English
Weight
468 KB
Volume
66
Category
Article
ISSN
0016-7037

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The transition from pyroxene granulite facies to garnet clinopyroxene granulite facies. Experiments in the system CaO-MgO-Al2O3-SiO2
✍ Birger Hansen 📂 Article 📅 1981 🏛 Springer 🌐 English ⚖ 903 KB

The pressure-temperature curve for the equilibrium anorthite + 2 enstatite = pyrope + diopside + quartz has been determined in the system CaO-MgO-A120 2 -SiO 2 to be between 13.4 and 14.0kbars at 900~ The slope up to 1,240~ is 8.5bar/K. The entropy change at 1,200K is 20kJ. These data, combined wit