陕西渭河盆地固市凹陷渭热2井组甲烷气成因及其意义

    The genesis of Methane in Weire 2 Well of Gushi Depression, Weihe Basin, Shaanxi Province, and its significance

    • 摘要: 渭河盆地固市凹陷渭热2井组甲烷气的成功点火,再一次引起人们对渭河盆地油气资源前景的关注。渭热2井组及邻区7口井天然气组分、甲烷C同位素等分析指标显示,该区甲烷气具有2种成因类型,浅部气层为新近系张家坡组生物成因气,中深部天然气来自前新生界煤型热解-裂解气;伴生CO2气为有机成因。地质分析认为,渭河盆地固市凹陷具有良好的新生界生物气资源前景,前新生界煤系地层也是渭河盆地重要的潜在烃源岩,表明渭河盆地具有开展进一步油气调查的资源基础。

       

      Abstract: The successful methane ignitions of Weire 2 well in Gushi Depression of Weihe Basin have drawn people's attention to the prospect of oil and gas resources in Weihe Basin again. Such analytical indices as natural gas components and methane carbon isotope of Weire 2 Well and its adjacent seven wells show that there are two kinds of genesis, i.e., Neogene biogenetic gas of Zhangjiapo Formation in the shallow part and Cenozoic coal pyrolysis gas in the middle and deep part. The indices also show that the associated CO2 is of organic origin. Geological analysis suggests that Gushi depression in Weihe Basin has a promising future of Cenozoic biogenetic gas, and pre-Cenozoic coal measures are important potential source rocks in Weihe Basin, which also provide source basis for further oil and gas survey in this area.

       

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