摘要
屯留井田以逆断层发育为特色，本文讨论了井田断层形态特征和断层展布规律，指出基底构造格局是控制本区煤田构造变形的基本因素，由此推断井田西部同样发育南北走向的逆断层。
The tectonic framework of Tunliu mine field is characterized by developing of re-verse faults. This paper deals with the form and distribution of faults in Tunliu mine field,confirms that the basement tectonic is a fundamental factor to.contro the cover strucutral de-formation. Based on the study of formation condition of reverse faults,the aut6ors infer thatN一Strended reverse faults may also distrbute in the west part of Tunliu mine field.
出处
《中国煤田地质》
1995年第2期7-10,共4页
Coal Geology of China
关键词
逆断层
屯留井田
断裂构造
煤矿床
Reverse faults Tunliu mine fild Structure forecast
