新疆尼勒克煤矿区六井田地质构造特征分析

Geological structural feature analysis for Nileke coal mining area six field in Xinjiang

文章查明了井田内断层F3断层、北部F2边界正断层和井田西部边界F6平移正断层的地质特征。井田地层为东西走向往北倾,呈南陡北缓的趋势,以19剖面线为分界线,东侧地层总体为一往北倾的单斜构造,西侧从18E、18、17E剖面北端逐渐变为一个向斜和一个背斜。

The feature of Fs fauh,nollhern F_, boundary normal faults and western boundary F6 translational normal fauhs of the coal field were identified in this paper. The stratigraphic occurrence of the field runs east-west and clines to the north ,with steep slope in the soulh and gentle slope in lhe north. 19 hatch is the dividing line,the east side of stratigraphy is a north dipping monoclinal structure overall, and lhe wes! side of it gradually lurns into a syncline and an anticline, from the north end of profile 1 BE, 18 and 17 E.