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Metamorphic Reactions in the Kyanite and Sillimanite Zones of the Barrovian Type Area 总被引:5,自引:1,他引:5
Metamorphic conditions in the staurolite, kyanite, and sillimanitezones of the Barrovian type area have been calculated usinga variety of equilibria. Temperatures ranged from 550?C (transitionzone) to 650?C (sillimanite zone) with P {small tilde} 6000bars and XH2O {small tilde} 0?6. Metamorphism was progressive,and the exact nature of the continuous reactions responsiblefor the formation of index minerals was strongly controlledby bulk rock Mg/(Mg + Fe). Thus, in magnesian rocks staurolitebroke down to kyanite + biotite, whereas in iron-rich rocksit broke down to garnet + muscovite and kyanite was not produced.Sillimanite formed both from kyanite and by dehydration reactionsof staurolite and white mica. 相似文献
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