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METAMORPHIC CORE COMPLEX IN GANZHUERMIAO, INNER MONGOLIA

Zhang Lüqiao (Geological Bureau of Inner Mongolia,Huhehaote 010020) Shao Ji'an (Peking University,Beijing,100871) Zheng Guangrui (Geoexploration Bureau of Inner Mongolia,Chifeng 024005)  
The Ganzhuermiao metamorphic core complex is found in the core of a quaquaversal anticalinoria in Da Hinngan Met.,composed of three parts:the core of Early Permian low amphibolite facies-high greenschist facies rocks with ductile deformation,the intermediate layer of Middle Jurassic sandrock slate with plasitic deformation and hornfelsing,and the overlying layer of Late Jurassic volcanic rocks,clastic rocks,and concurrent granite with brittle deformation but without metamorphism. Detachment surfaces exist between the above mentioned parts.The extensional lineations in the flat slip planes and associated folds show that the layers abovethe detachment surfaces slipped downward NW and SE symmtrically and the underlying blocks detached continuously and rised to the superficial layer when the metamorphic core complex was upwelling,whereas the ultramafic mafic rocks intruding into the core were exhumed. It is inferred from the difference between the respective metamorphism and deformation characterstics of the Middle and Late Jurassic formations that thermal metamorphism of the metamorphic core complex occurred at the end of the Middle Jurassic,and that its abrupt rising and the downward sliding of the overlaying layers happened at the end of the Late Jurassic or at the Early Creataceous. It is the thermal uplifting that caused extension but not on the contrary.
【Fund】: 国家自然科学基金
【CateGory Index】: P588.34
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