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医巫闾山变质核杂岩构造特征
引用本文:马寅生,崔盛芹,吴淦国,吴珍汉,朱大岗,李晓,冯向阳.医巫闾山变质核杂岩构造特征[J].地球学报,1999,20(4):385-391.
作者姓名:马寅生  崔盛芹  吴淦国  吴珍汉  朱大岗  李晓  冯向阳
作者单位:中国地质科学院地质力学研究所,北京;中国地质科学院地质力学研究所,北京;中国地质大学,北京;中国地质科学院地质力学研究所,北京;中国地质科学院地质力学研究所,北京;中国地质科学院地质力学研究所,北京;中国地质科学院地质力学研究所,北京
基金项目:地矿部九五重点科技项目《燕山造山带造山作用过程及动力学机制》
摘    要:经过野外宏观观测、室内显微分析及同位素年龄测定,基本厘定医巫闾山是一个白垩纪时形成的变质核杂岩。变质核杂岩中心为晚燕山期的医巫闾山二长花岗岩体,周围是由代表地壳深部变形特点的太古宇变质岩组成的变质核。变质核北面和东面以拆离断层与盖层下部中新元古界相接触,并为中新元古界组成的韧性流变的中间层所环绕。变质核西面以阜新盆地东南缘边界正断层( 孙家湾- 稍户营子正断层) 与盖层上部以脆性变形为特征的白垩纪碎屑岩相邻。变质核杂岩的变形片理、线理及运动指向说明该变质核杂岩为对称型变质核杂岩。

关 键 词:变质核杂岩  医巫闾山

The Structural Feature of Metamorphic Core Complex in Yiwülshan Mountains,West Liaoning
MA Yin-sheng,CUI Sheng-qin,WU Jin-guo,ZHU Zhen-han,ZHU Da-gang,LI Xiao and FENG Xiang-yang.The Structural Feature of Metamorphic Core Complex in Yiwülshan Mountains,West Liaoning[J].Acta Geoscientia Sinica,1999,20(4):385-391.
Authors:MA Yin-sheng  CUI Sheng-qin  WU Jin-guo  ZHU Zhen-han  ZHU Da-gang  LI Xiao and FENG Xiang-yang
Affiliation:Institute of Geomechanics, CAGS, Beijing;Institute of Geomechanics, CAGS, Beijing;China University of Geosciences, Beijng;Institute of Geomechanics, CAGS, Beijing;Institute of Geomechanics, CAGS, Beijing;Institute of Geomechanics, CAGS, Beijing;Institute of Geomechanics, CAGS, Beijing
Abstract:Yiwulüshan mountain is proved to be a metamorphic core complex formed in Cretaceous according to field survey, microstructural analysis, and isotropic dating. The center of the metamorphic core complex is Yiwulüshan Late Yanshanian adamellite. The metamorphic core consists of Archaean metamorphic rock which represents ductile deformation in the crust deep and surrounds the Yiwulüshan adamellite. The lower part of the cover layer consists of Middle and Upper Proterozoic,spreads in the northern part and the eastern part of the metamorphic core and connects with the metamorphic core by a detachment fault. It is cut by Sunjiawan-Saohuyingzi normal fault in the west of the metamorphic core. The metamorphic core complex is considered to be symmetric type metamorphic core complex in the light of deformation schistosity, lineation, and the indication of the shear movement.
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