A fter comprehens ive resea rch on the form ation cond ition and d istr ibution law of Reheta i o il layer reservo ir in the Q i- Shuang area, the conclusion is that the m a in reservo ir in the Q ijia ram p reg ion is "Foliaceous" litho log ic reservo ir. The oil and gas in the sou th o f this a rea is sufficien t. The depo sition o f sand in the no rth is sequentia ,l but on ly some sing le layer reservo ir is fo rm ed in the no rth. The ma in reservo ir in the Shuangta izi anticlinal belt is struc tura l hydroca rbon reservo ir, and o il m ainly accumu la tes in the ax ial reg ion of the anticline. The o il accum ulation is reso lved by the area and closure of block fau lt, thickness and physical property o f reservo ir. Based on the o il d iffe rentia l accumu lation theory, the m a in agg regation in the Shuang taizi anticlinal be lt is gas and o il in the Q ijia ramp reg ion. W ate r is in the a rch bend. The arch bend is the m a in m igration path, but there is not preservative cond ition.
关键词:
齐- 双地区 热河台油层 油气藏形成 油气分布;
Keywords:
Q i- Shuang area, Rehetai o il form ation, reservo ir forma tion, o il and g as distr ibution.;