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- W2509478410 abstract "For the first time, we find kyanite-topazite which is similar to the white schist from abroad, in aiangsu, Anhui, Henan of China. Because of intercontinental obduction and collision, the kyanite-topazite is formed from the superhigh-pressure metamorphism of sedimentary rock in continental crust, at the depth of mantle. Kyanite-topazite runs parallel to blue schist, eclogite and constitutes the high-pressure metamorphic belt in Central China. Its original rocks are a set of sedimentary rock series which is mainly composed of marginal shallow marine facies to continental facies pelitic to magnesium carbonatite, both rocks exist in Precambrian Middle-Upper Proterozoic metamorphic strata." @default.
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- W2509478410 date "1993-07-20" @default.
- W2509478410 modified "2023-09-23" @default.
- W2509478410 title "The Discovery and Geological Feature of Kyanite-Topazite in High-Pressure Belt From Central China" @default.
- W2509478410 doi "https://doi.org/10.1360/ya1993-36-7-856" @default.
- W2509478410 hasPublicationYear "1993" @default.
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