摘要
涟源含煤区（简称本区）发育有北东向和北西向两组基底断裂构造,该基底断裂构造将本区分割成若干微断块,本区盖层构造受基底构造控制明显，不同的盖层构造样式，与由基底断裂所固限的特殊微断块相对应。
Lianyuan Coal-Bearing Strata（LCS） consists of two basement faults： one is in the northeast and the other in the northwest. They together divide LCS into many minor--faults. Research shows that the basement construction distinctively controls the capping construction and different capping constructions correspond to specific minor--faults confined by the basement faults.
出处
《株洲师范高等专科学校学报》
2005年第5期18-20,36,共4页
Journal of Zhuzhou Teachers College
关键词
基底断裂构造
盖层构造
微断块
basement construction fault capping construction minor--fault
