Sudeerte tectonic zone research, through the production of the forty wells synthetic seismograms, accurate calibration of each structural layers and the corresponding relationship between seismic reflections. According horizon calibration, determine the T5 reflective layer is reflective top surface bedrock Budate group, and the overlying strata Mountains form a strong earthquake in the region to respond. By variance cube slice and layer slices along better identification of faults and fault distribution characteristics and laws. By creating layers and structural composite structure diagram graph to determine the area of structural characteristics and tectonic evolution. By constructing the characteristics of the deep rift with the bedrock structure raised by the control, showing two concave clip a long tectonic pattern, that is, from north to south of Rabaul Tolgoi syncline Sudeerte uplift, Ao mind syncline Long alternating concave presented. Developmental history of tectonic rift mainly for Bell as well as apparent Hailar Basin basement fault-controlled, multi breaking off small Au Au transitional basins.
Profile of regional tectonic characteristicsBy high resolution 3 d seismic data interpretation, the implementation of the different reservoir top surface structure and fault development situation, find out the characteristics of tectonic development [1]. Steve souders buir lake depression structural belt is located in hailaer basin, belongs to the sag in the eastern fault terrace zone, the geographical position in Inner Mongolia autonomous region within the territory of surveillance, Steve souders, tectonic belt hinggan mountains oil layer on the surface of the roof structure of the bei 10, 12, bei bei 14, 20, bei bei 16 Wells in a line from north to east of relatively complete arched structure, including oil Wells are distributed on the uplift belt, inheritance of deep large faults developed in the edge of the uplift belt, uplift area form relatively favorable structural trap. Throughout the main development of the hinggan mountains near the north east and near north-south fault, the fault cutting each other, make further complicate structure, forming the block structure of different sizes.The top surface of Budate reservoir is mainly uplift to the North East, where along the Bay in 12, 14, 20, Bei Bei Bei 16 area development main uplift belt, development of a secondary uplift along the Bay 22, Bei 16 area. The main uplift belt distribution of multiple oil-bearing fault blocks, are distributed in the main uplift zone flow well sude Erte area industrial oil. The area is mainly developed in the North East fracture, substantially parallel to the uplift, the maximum displacement of 800m, 15km in the maximum extended length. In the edge uplift belt, fractures are most developed.The Sudheer Te tectonic belt of Xingan Ling reservoir types are sandstone and conglomerate, tuff, tuffaceous sandstone and conglomerate, and tuffaceous conglomerate, glutenite reservoir has strong sensitivity. Budate reservoir for the slight...