南黄海海相中—古生界碳酸盐岩储层特征及成藏模式——对比四川盆地和苏北盆地

    CHARACTERISTICS OF MESOZOIC-PALAEOZOIC MARINE CARBONATE RESERVOIR IN THE SOUTH YELLOW SEA BASIN AND HYDROCARBON ACCUMULATION:COMPARISON BETWEEN THE SICHUAN BASIN AND THE SUBEI BASIN

    • 摘要: 通过对比四川盆地、苏北盆地和南黄海盆地的钻井、测井、岩心、野外露头等资料,分析了南黄海中—古生界海相碳酸盐岩储层类型及其成藏模式。研究区存在白云岩孔隙储层、礁滩相储层、风化壳储层和裂隙储层,成藏模式有威远式、安岳式、五百梯式和普光式,并且预测南黄海崂山隆起具备以上4种成藏模式,为目前及将来勘探的重点目标。

       

      Abstract: Comparison of drilling, logging, core and outcrop data is made for the Mesozoic and Paleozoic carbonate reservoir in the Sichuan Basin, Subei Basin and the South Yellow Sea Basin, in order to reveal the similarities and differences of hydrocarbon accumulation in these basins. There are four kinds of reservoirs in this region, i.e. the porous dolomitic reservoir, reef-bank reservoir, weathering crust reservoir and fractured reservoir, and four kinds of hydrocarbon accumulation, namely the Weiyuan type, the Anyue type, the Wubaiti type and the Puguang type. It is predicted that the four types of hydrocarbon accumulation may all occur on the Laoshan Uplift of the South Yellow Sea Basin.

       

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