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运用遥感和地学信息探讨华北地台北缘边界断裂
引用本文:邓兆伦,曹书静,崔新省.运用遥感和地学信息探讨华北地台北缘边界断裂[J].国土资源遥感,1995,6(2):15-22.
作者姓名:邓兆伦  曹书静  崔新省
作者单位:地矿部航空物探遥感中心,中国地质大学
摘    要:华北地台北缘与兴蒙褶皱系的界线为一深大断裂带,属于一级大地构造单元之间的界线。笔者通过对覆盖全区50万km2陆地卫星TM图像解译,参考重力、航磁及有关地质资料,结合笔者对其不同区段的野外调查,对此断裂带的展布位置、性质及其控矿作用取得了一些新的认识。

关 键 词:遥感  地学信息  华北地台  北缘  断裂
收稿时间:1993-12-10

THE COMPREHENSIVE INQUIRE INTO THE BOUNDARY FAULT OF NORTH CHINA PLATFORM'S NORTH MARGIN BY REMOTE SENSING AND GEOSCIENCE
Institution:1. Center for Remote Sensing in Geology, MGMR, Beiging, 100083;
2. China University of Geosciences, Beijing, 100083
Abstract:The boundary between North China platform's North margin and XinganNei Mongol fold system,is a deep and great fault zone, which is the kind of boundary between the largest geotectonic units on the Earth Surface.The authors interpreted the landsat TMimages of an area of 4×105 km2 of this zone, referred to gravity and air-magnetic survey and other related geological data, and took into consideration their previous field surveys of different parts of the zone, thus got some new understanding about the stretch position,Nature and ore control of this fault zone.
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