东至断裂在查册桥一带构造特征及其地质意义  

Structural characteristics and geological significance of Dongzhi fault in the area of Chajingqiao

作　　者：罗红波[1] 沈欢喜[1] 钱祥[1] 陈金苗[1] 孙鹏艳 LUO Hong-bo;SHEN Huan-xi;QIAN Xiang;CHEN Jin-miao;SUN Peng-yan(geological team of Anhui Bureau of Geology and mineral exploration,Anqing 246003,China)

机构地区：[1]安徽省地质矿产勘查局311地质队,安徽安庆246003

出　　处：《世界有色金属》2021年第6期227-228,共2页World Nonferrous Metals

摘　　要：近年来关于东至断裂构造特征及控岩控矿方面的调查和研究很多,但其在北部查册桥一带与高坦断裂复合部位的构造特征研究较少,笔者通过大量的野外调查,发现东至断裂主断层在查册桥北东侧太阳坞一带为晚期滑覆构造掩盖。In recent years,there have been a lot of investigations and studies on the structural characteristics of the Dongzhi fault and its rock and ore control,but few studies on the structural characteristics of the composite part with Gaotan fault on the north in Zhaceqiao area.Through a lot of field investigations,the author found that the main fault of the Dongzhi fault in the Taiyangwu area on the northeast side of Chazhenqiao is covered by the late slip overburden structure.

关 键 词：东至断裂 高坦断裂 推覆-滑覆体系 

分 类 号：P548[天文地球—构造地质学]