ABSTRACT
The mining area is located in the oblique east wing of the back of Xibeikulasi, and is relatively flat, which belongs to the low mountain hilly terrain. The altitude is 770 meters, the relative elevation is generally of 5 to 15 meters, and the scope of mineralization is an oval area with the length and width of about 1.0 km. The exposed stratum is Xibeikulasi Shangya Formation (C1X2) and Baogutu Xiaya Formation (C1B1) of Lower Carboniferous Series. The stratum is in nearly north-south direction, with tendency to the east and the dip angle of 60° to 70°.
