The studies show that the sandstone reservoirs of the buried hills of jurassic in baigezhuang region developed three groups of fractures , which most tend towards in ne ( nee )
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There are three patterns of lateral enclose for the faults of buried hill chegu 20 : sealed by lithology joint , sealed by shale - smear and sealed by high displacement pressure in fault zone
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Richly accumulative zones of oil - gas in carbonate rocks have three types : huge upheavals , organic mounds and buried hills . the paper mainly discusses carbonate reservoir in buried hills
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2 . it is the first time to divide the structure of qianmiqiao buried hills into three structural layers : buried hills thrust fault block , paleogeomorphic relict mountain and lowland , tilting horst block
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On the basis of all kinds of fracture data , the characters of the buried hill reservoirs of mesozoic are considered as fracture - pore dual mediums , and then the hydrocarbon reservoir was predicted
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It is the regional structure stress field formed in the processes of formation of the major faults of buried hills action on the graben that controlled the development of the fractures of sandstone of mesozoic of baigezhuang region
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6 . the character of hydrocarbon production and high gas - oil ratio show that the main migration facies in buried hills is gas facies ( including condensed gas facies ) . the early migration facies is condensed gas facies , later , gas facies
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