THE PRESSURE-TEMPERATURE-SPACE-TIMECPTSt EVOLUTION OF METAMORPHISM AND DEVELOPMENT MECHANISM OF THE THERMAL-STRUCTURAL-GNEISS DOMES IN THE CHINESE ALT AIDES
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Abstract:
During the main episode of the Chinese Altaides (Early Carboniferous), progressive metamorphic zones, migmatite zones and migmatitic granitic gneiss fileds developed around and in the regional thermodynamic anomalies in the orogenic belt and constitute a
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Zhuang Yuxun.1994. THE PRESSURE-TEMPERATURE-SPACE-TIMECPTSt EVOLUTION OF METAMORPHISM AND DEVELOPMENT MECHANISM OF THE THERMAL-STRUCTURAL-GNEISS DOMES IN THE CHINESE ALT AIDES[J]. Acta Geologica Sinica,68(1):
