准噶尔盆地北三台地区三叠系克拉玛依组沉积相研究

ccording to a large number of core observation, seismic and Well logging data, we divided T2k into two systems tracts in the region called Beisantai in Junggar Basin. And On this basis, we researched the sedimentary facies about T2k.We did sedimentary facies of single well and sedimentary facies of connection wells in the same direction, we also did equal line map of sandstone thickness, conglomerate thickness, sandstone content and then we drew the map of the distribution of sedimentary facies about T2k. Therefore, these maps have isochronous, causes of continuity and availability, and also can effectively overcome the same-phase deposition of this difficult issue of comparing. It is good to provide the basis for the Oil and Gas Exploration.