“滑动残留岩体”的特征及其找矿意义  

"Sliding Relict" Characteristics and Its Prospecting Importance

作　　者：戴定贤[1] 

机构地区：[1]福建省197煤田地质勘探队,福建泉州362000

出　　处：《中国煤炭地质》2006年第6期9-10,共2页Coal Geology of China

摘　　要：福建省童子岩组含煤岩系的上部及下部常发育有一组滑脱断层,它常常造成地层缺失,并在其滑动断裂带上残留下岩块,这就是所谓的“滑动残留岩体”。通过分析“滑动残留岩体”的特征来指导研究区地质找矿工作。In the upper and lower parts of Tongziyan Formation coal-bearing strata in Fujian Province,there has often a set of decollement that usually causing strata hiatus.Furthermore,frequently it may leave rock blocks on the glide zones,what is we termed ″sliding relict″.Then we use it in our prospecting works through analyses of the ″sliding relict″.

关 键 词：滑脱断层 滑动残留岩体 特征 童子岩组 

分 类 号：P542.3+.3[天文地球—构造地质学]