首页 | 本学科首页   官方微博 | 高级检索  
     检索      

一条早前寒武纪的陆-陆碰撞造山带——华北克拉通北缘中西部麻粒岩相带
引用本文:赵靖,钱祥麟.一条早前寒武纪的陆-陆碰撞造山带——华北克拉通北缘中西部麻粒岩相带[J].地质科学,1996,31(4):342-352.
作者姓名:赵靖  钱祥麟
作者单位:1. 中国地质大学地质系, 北京 100083;2. 北京大学地质系, 北京 100871
基金项目:国家自然科学基金(项目号:49302036),博士后基金
摘    要:详细的野外调查、原岩建造、变质作用、变形作用以及同位素年代学研究表明,华北克拉通北缘中西部麻粒岩相带是我国迄今能识别的最老的陆-陆碰撞造山带的根带,可与世界上著名的南非Limpopo碰撞造山带对比。

关 键 词:麻粒岩相带  早前寒武纪  碰撞造山带  高温韧性剪切带
收稿时间:1994-05-12
修稿时间:1994-05-12;

A GRANULITE FACIES BELT OF THE MIDDLE-WEST PART EN NORTH MARGIN OF NORTH CHINA CRATON: AN EARLY PRECAMBRIAN CONTINENT- CONTINENT COLLISION OROGENIC BELT
Zhao Jing Qian Xianglin.A GRANULITE FACIES BELT OF THE MIDDLE-WEST PART EN NORTH MARGIN OF NORTH CHINA CRATON: AN EARLY PRECAMBRIAN CONTINENT- CONTINENT COLLISION OROGENIC BELT[J].Chinese Journal of Geology,1996,31(4):342-352.
Authors:Zhao Jing Qian Xianglin
Institution:1. Department of Geology, China University of Geosciences, Beijing 100083;2. Department of Geology, Peking University, Beijing 100871
Abstract:The cumulative geological data from detailed field mapping and the analyses of protolith formations, metamorphism, deformation and isotopic chronology of granulite facies rocks show that a granulite facies belt of the middle-west part in north China craton is probably recongnised to be an Early Precambrian continent-continent collision orogenic belt. It is due to collage between north China paleo-plate and Iner Mongolian paleo-plate. This belt can be compared to Limpopo belt of well-known Early Precambrian collision belt over the world.
Keywords:Granulite fades belt  Early Precambrian  Collision orogenic belt  High-temperature ductile shear zone
本文献已被 CNKI 维普 等数据库收录!
点击此处可从《地质科学》浏览原始摘要信息
点击此处可从《地质科学》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号