摘要
介绍了研究区及周围地区的构造背景 ,对宏观与微观构造进行了深入研究 .结果认为 :研究区自晚古生代煤系地层形成以来 ,经历了多期构造事件 ,主要有三期构造应力场的更替 ,形成了复杂的断块构造 .特别是新生代晚期以来的地壳运动 。
Geological setting of the research area as well as its surrounding fields was introduced; The macro and micro structures were researched in detail. The result shows that , since the coal measures formed in Late Paleozoic, the research area has been undergone several tectonic events; Three stress fields have been formed alternatively, resulting in forming a complex faulted block structure. The tectonic movement since Late Cenozoic has important effects on the structural framework of coal fields and the distribution of coal measures in the middle Shanxi Province.
出处
《中国矿业大学学报》
EI
CAS
CSCD
北大核心
2001年第5期463-466,共4页
Journal of China University of Mining & Technology
基金
山西省煤田地质局科研项目<樊王普查区构造特征研究>的部分成果
关键词
晋中断陷
樊王普查区
断块构造
构造演化
Jinzhong fault depression
faulted block structure
tectonic evolution
