一、地质概况淄博煤田位于华北地台东部的鲁西台背斜北侧,为一走向北东的单斜构造,倾向北西。临淄勘探区位于淄博煤田东北部,区内构造复杂,岩浆岩发育,地层倾角一般在15°以内。本区地层属于典型的华北型,由老到新有奥陶系、石炭系、二叠系,第三系和第四系分布较普遍。主要含煤地层为上石炭统太原 I. Geological Survey Zibo Coalfield is located on the north side of Luxi Taiwan anticline in the eastern part of North China Platform. It is a monoclinic structure that runs to the east and tends to be northwest. Linzi exploration area is located in the northeast of Zibo Coalfield, the structure of the complex, rock development, stratigraphic dip generally within 15 °. The strata in this area belong to the typical North China type. The Ordovician, Carboniferous, Permian, Tertiary and Quaternary systems are widespread from old to new. The main coal-bearing strata are Upper Carboniferous