鄂尔多斯盆地煤油气共生矿井中原油来源及时空演化以芦村矿区为例

Origin and spatial-temporal evolution of crude oil in coal-oil-gas symbiotic mines in Ordos Basin:Taking Lucun mining area as an example

  • 摘要: 鄂尔多斯盆地南部大量矿井均有煤油气共生情况,煤矿开采过程中从其顶底板泄漏的原油为煤矿开采带来了巨大安全隐患,因此需进一步明确其原油来源及时空演化。以盆地南部芦村矿区延安组为研究对象,系统采集了煤系烃源岩及工作面原油样品,进行了有机碳同位素和气相色谱质谱等测试,分析了烃源岩及原油的碳同位素和生物标志化合物特征,探究了矿区内延安组原油的来源。通过查明矿区内断裂体系,探讨了断裂形成时代,结合区域应力场特征,综合揭示了鄂尔多斯盆地南部延安组煤矿中泄露原油的时空演化。结果表明:延安组煤矿中的原油来源于下伏三叠系延长组长7烃源岩;矿区内发育的北东向大断层,是受印支期构造应力影响,后经过燕山和喜山期构造运动改造调整形成的一个Ⅱ级断层,该断层为原油由延长组向延安组运移提供了主要通道;矿区内发育的东西向小断层主要受控于燕山中晚期北西西—南东东向水平挤压应力,东西向节理主要受控于喜山期北北西—南南西向应力作用,二者均为延安组煤矿开采过程中原油散逸的主要路径。早白垩世延长组长7烃源岩开始大量生烃,形成的原油沿着北东向大断层运移至延安组,最终通过东西向的小断层和节理流入矿井。研究结果可为煤油气共生矿井中原油泄露的防治及安全开采提供理论指导。

     

    Abstract: A large number of mines in southern Ordos Basin have coal-oil-gas symbiosis, and the crude oil leaking from the top and bottom of the coal mining process has brought great security risks to the coal mining, so it is necessary to further identify the source and space-time evolution of the crude oil. Yan’an Formation in Lucun mining area in the southern basin was selected as the research object. Samples of coal measure source rocks and working face crude oil were systematically collected, and organic carbon isotope and gas chromatography-mass spectrometry were conducted to analyze the carbon isotope and biomarker characteristics of source rocks and crude oil, and the source of Yan’an Formation crude oil in the mining area was explored. By identifying fault system in the mining area, formation time of the fault is discussed, combined with characteristics of regional stress field, temporal and spatial evolution of the oil leakage in Yan’an Formation coal mine in southern Ordos Basin is comprehensively revealed. The results show that: Crude oil in Yan’an Formation coal mine comes from lower Triassic Yanchang 7 source rock; NE-trending large fault developed in the mining area is a class II fault, which was formed by the tectonic stress of Indosinian period and then reformed by Yanshan and Himalayan tectonic movements. This fault provides the main channel for the migration of crude oil from Yanchang Formation to Yan’an Formation; Small EW trending fault developed in the mine is mainly controlled by NWW-SEE horizontal compressive stress in the middle and Late Yanshan period, and EW trending joint is mainly controlled by NNW-SSW trending stress in Mountain Age, both of which are the main paths of crude oil escape in the coal mining process of Yan’an Formation. In Early Cretaceous, source rock of Chang 7 Yanchang began to generate a large amount of hydrocarbon, and the formed crude oil migrated to Yan’an Formation along NE trending large fault, and finally flowed into the mine through EW trending small fault and joint. The research results can provide theoretical guidance for the prevention and control of crude oil leakage and safe exploitation in coal-oil-gas symbiotic mine.

     

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