左云陈家堡位于大同煤田西北部,处于华北地台的北部边缘,各期地层有许多特殊之处。石炭系上统太原组以三角洲陆相沉积为主的含煤地层,基本上见不到海相灰岩。海相泥岩、泥灰岩也只在南部见到一层。碎屑岩特别发育,煤层较厚。燕山运动是它形成的决定时期。沿东缘发生的口泉—鹅毛口逆推断裂,使煤田以东太古界的上覆地层全部遭受剥蚀,因推覆、挤压,使煤田西、北部平缓上升,遭受剥蚀、侵蚀;侏罗系末期的唐河断裂,使西北部复又快速下沉,并为白垩系巨厚沉积所覆盖;喜山运动再次沿口泉山脉东麓发生强烈断陷,形成大同断陷盆地。 Zuoyun Chenjiapu is located in the northwestern Datong Coalfield, on the northern margin of the North China platform. There are many specialties in each stage. The Carboniferous Upper Tertiary Formation is mainly composed of deltaic continental sedimentary coal-bearing strata, and basically can not see marine limestone. Marine mudstone and marl also see only one layer in the south. Clastic rock is particularly developed, thick coal seam. Yanshan movement is the decisive period of its formation. The mouth spring-goose-feather fracture along the eastern edge of the coal seam reverse thrust fracture, so that the overlying strata in the Archean boundary east of the coal field are all eroded, because of nappe, squeeze, so that the coal field gently rose in the west and north, suffered erosion, erosion; Jurassic The end of the Tanghe fault, so that the northwestern complex rapid subsidence and thick Cretaceous sedimentary cover; Himalayan movement once again along the mouth of the mouth of the mountains occurred a strong fault depression, the formation of the Datong fault basin.