XIA Mingjun; DAI Jinxing; ZOU Caineng; WANG Zecheng and TAO Shi-zhen
, 2007, 34(3): 1477-0.
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The distribution of Caledonian residuum reservoirs in the south of Ordos Basin is mainly controlled by karst palaeogeomorphology, strata of residuum and sedimentary facies. The facies of the O1m5 residuum is dolomitic tidal flats, with well-developed dissolved pores; while that of O2p is deep water slopes, with abundant faults, fractures and caves. On the central palaeohigh, palaeogeomorphology is platforms composed of old strata and compacted rock, with vertical fractured zones at the residuum's top; on the west side, it is slopes with well-developed fractures and caverns; on the south side, it is platforms with well-developed faults, caverns, and weathering fractures; on the east side, it is mostly terraces or saddle-shaped terrain, with abundant dissolved pores in the residuum which locates on dolomitic or anhydrite-bearing dolomitic tidal flats. The main controlling factors of the forming of gas pool are hydrocarbon generating center, palaeogeomorphology, strata of residuum and sedimentary facies. Favorable zones are the O2p hydrocarbon generating center in Yaoxian, Xunyi and Chunhua and the O1m5 in eastern central palaeohigh.