从高丽营探槽分析黄庄—高丽营断裂与地裂缝的关系  

The Relation Between Huangzhung-Gaoliying Fault and By Gaoliying Trench and Earth Fissure

作　　者：贾三满[1] 郭萌[2] 

机构地区：[1]北京市地质环境监测总站,北京100037 [2]北京市地质矿产勘查开发局,北京100050

出　　处：《城市地质》2007年第4期24-28,共5页Urban Geology

摘　　要：高丽营探槽揭示的地质现象表明,黄庄—高丽营断裂错断全部第四系地层,断裂面直达地表,累计断距约1.5m左右。黄庄—高丽营断裂的地表断面位置与地裂缝完全一致,与已造成较大损失的高丽营地裂缝关系密切,说明黄庄—高丽营断裂目前仍在活动。The geological phenomenon explored by Gaoliying trench indicates that Huangzhuang- Gaoliying fault breaks completely Fourthly Series stratum, and reaches the earth＇s surface directly, and the fault throw has reached 1 .Sm in total. The consistent of Huangzhuang-Gaoliying fault to the earth surface and the earth fissure, and the relation between Huangzhuang-Gaoliying fault and Gaoliying earth fissure which has cause great economic loss shows that Huangzhuang-Gaoliying fault is still being active.

关 键 词：活动断裂 地裂缝 探槽 

分 类 号：P542[天文地球—构造地质学]