凝析油气富集带的地质特征１．轮台断隆的地质结构轮台断隆是塔北古生代残余古隆起的核心，是受英买７号—轮台大断裂和牙哈大断裂控制的断垒块体。上述两条大断裂在古生代呈背冲式逆断层，到了中生代反向活动，在其上方派生出两组正断层。轮台断隆南侧是塔北隆起的南斜坡... Geological Features of Condensate Hydrocarbon Enrichment Belt 1. The rupture of the bedrock formed by the rupture of the Longtai platform is the core of the Paleozoic remnant palaeo uplift in the North Paleozoic. It is a block fault ruled by Yingbashi No. 7 - the Grand Rift Fault and the Yahada big fault. The two major faults were backflush reverse faults in the Paleozoic, and to the Mesozoic reverse activity, two sets of normal faults were derived from above. Rotary Tai Long south of the tower is uplift of the southern slope ...