赣北中元古界双桥山群低变质强变形行为与格林威尔期造山作用 STUDY ON THE BEHAVIOUR OF THE LOW-GRADE METAMORPHI

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赣北中元古界双桥山群低变质强变形行为与格林威尔期造山作用

STUDY ON THE BEHAVIOUR OF THE LOW-GRADE METAMORPHISM AND HIGH DEFORMATION OF THE MIDDLE PROTEROZOIC SHUANGQIAOSHAN GROUP IN NORTH JIANGXI AND GRENVILLE PHASE OROGENY

广泛分布于赣北地区的中元古界双桥山群,以低级区域变质作用、强烈构造变形、具陆内造山带构造变形特征;其成因系在华夏古陆与扬子古陆的碰撞拼接过程中,其应力向陆内传递的结果;时间大致在1 100~800 Ma,与全球格林威尔期造山作用相当.水利论文Bt_BPz#Q

作 者: 秦松贤 章泽军 张志 赵温霞 蔡雄飞 顾延生  
作者单位:中国地质大学地球科学学院,湖北,武汉,430074 
刊 名:地质科技情报  ISTIC PKU
英文刊名:GEOLOGICAL SCIENCE AND TECHNOLOGY INFORMATION 
年,卷(期):2002 21(2) 
分类号:P542.2 
关键词:赣北   中元古代   双桥山群   低级变质   强烈变形   格林威尔  
机标关键词:赣北地区中元古界双桥山群变质作用变形行为格林威尔期造山作用MIDDLE PROTEROZOIC构造变形陆内造山带华夏古陆变形特征应力区域拼接碰撞分布成因 
基金项目:国家地调项目 
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