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峰峰煤田地处太行山东麓中段,北至南洺河,南至漳河,西靠太行山,东接河北平原,呈一南北向的狭长地带。煤田中部有鼓山横贯南北,将煤田分为鼓山东西两块。 煤田地质构造型式主要为褶曲与断裂。大的构造有煤田西部的太行山隆起、煤田中部的鼓山复背斜、鼓山西和村—孙庄向斜和鼓山东单斜。煤田内断层极发育,纵横交错将煤田切割、破坏成许多次一级的构造块段,成为煤田矿井井田划分的天然边界(图1及图2)。
Fengfeng Coalfield is located in the middle of the eastern foot of Taihang Mountains, north to the Nanxun River, south to Zhanghe, Taihang Mountain in the west and Hebei Plain in the east, showing a narrow strip of north-south direction. Drum Hill in the central part of the coal field runs north and south, dividing the coalfield into two blocks of Gushan Mountain. Coal geological formations are mainly folds and faults. Large structures include the Taihangshan uplift in the western part of the coalfield, the Gushan anticlinorium in the middle of the coalfield, the western and village Gushan-Sunzhuang syncline and the Gushan Shan monoclinic. The faults in the coalfield are extremely developed. The coal fields are cut in a criss-cross pattern to destroy many structural blocks and become the natural boundaries of minefields in coalfields (Figure 1 and Figure 2).