A petrogenetic grid for pelitic schists in the system SiO 2 -Al 2 O 3 -FeO-MgO-K 2 O-H 2 O

作者: Frank S. Spear , John T. Cheney

DOI: 10.1007/BF00375302

关键词: BiotiteGeologyAndalusiteSillimaniteKyaniteCordieriteStauroliteAnalytical chemistryMuscoviteMineralogyChloritoid

摘要: A quantitative petrogenetic grid for pelitic schists in the system KFMASH that includes the phases garnet, chlorite, biotite, chloritoid, cordierite, staurolite, talc, kyanite, andalusite, …

参考文章(45)
Akiho Miyashiro, Metamorphism and Metamorphic Belts ,(1973)
D. Norton, R. Knapp, Transport phenomena in hydrothermal systems: the nature of porosity American Journal of Science. ,vol. 277, pp. 913- 936 ,(1977) , 10.2475/AJS.277.8.913
M. J. Holdaway, Stability of andalusite and the aluminum silicate phase diagram American Journal of Science. ,vol. 271, pp. 97- 131 ,(1971) , 10.2475/AJS.271.2.97
Frank S. Spear, Thermodynamic projection and extrapolation of high-variance mineral assemblages Contributions to Mineralogy and Petrology. ,vol. 98, pp. 346- 351 ,(1988) , 10.1007/BF00375184
Peter O. Koons, Alan B. Thompson, Non-mafic rocks in the greenschist, blueschist and eclogite facies Chemical Geology. ,vol. 50, pp. 3- 30 ,(1985) , 10.1016/0009-2541(85)90109-3
CHARLES V. GUIDOTTI, Transition from Staurolite to Sillimanite Zone, Rangeley Quadrangle, Maine Geological Society of America Bulletin. ,vol. 85, pp. 475- 490 ,(1974) , 10.1130/0016-7606(1974)85<475:TFSTSZ>2.0.CO;2