Mineralogy and Metamorphism of the Changqiang Metamorphic Dome
详细信息   
摘要
The Cangqiang dome is one of typical metamorphic domes in the Danba-Muli belt on the west margin of the Yangtze Platform. 4 metamorphic stages may be divided in the metamorphic dome on the basis of mineralogy and metamorphism. Imperfect coincidence of spotted mangan-almandite zone and progressive metamorphic zone with structural zonation of the dome and higher geothermal gradient in the principal metamorphic stage indicate that the Changqiang metamorphic dome is a tectonic-thermal one.

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