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首页> 外文期刊>Arabian journal of geosciences >Coal-measure source rock characteristics and burial evolution history in the Shisanjianfang Area, Tuha Basin
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Coal-measure source rock characteristics and burial evolution history in the Shisanjianfang Area, Tuha Basin

机译:吐哈盆地十三尖房地区煤系烃源岩特征及埋藏演化历史

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Shisanjianfang Area in the eastern margin of Taibei Sag, Tuha Basin, is an important region for oil and gas exploration. In this study, a large number of source rock geochemical data were used to analyze the geochemical characteristics of coal-measure source rocks in the Shisanjianfang Area, Tuha Basin, from three aspects, i.e., organic matter abundance, organic matter type, and organic maturity. The results show that the Jurassic Xishanyao Formation (J(2)x) in the study area has great thickness, continuous distribution, and high source rock maturity, and is the major source rock horizon in the study area. The seismic data are used in combination with 1D and 2D basin simulation technology to study the distribution characteristics of the source rocks in Shisanjianfang Area. The results of the simulation research on the source rock maturity history in the study area indicate the following: (1) The source rocks in the Xishanyao Formation (J(2)x) have a hydrocarbon generation threshold depth of 1800 m, threshold temperature of 95 degrees C, and hydrocarbon generation threshold time of about 162 Ma. (2) The Xishanyao Formation (J2x) has a current formation temperature of 50 similar to 110 degrees C and Ro of 0.6 similar to 1.1 % in the peak oil generation stage. (3) The source rock maturity in the study area is shown as being higher in the west while lower in the east, and higher in the north while lower in the south, and the favorable exploration area mainly lies in the northwest of the study area. The results of this study could have important implications for the oil and gas exploration in the margins of Xiaocaohu Sag, Tuha Basin.
机译:吐哈盆地台北凹陷东缘的三尖尖坊地区是油气勘探的重要地区。本研究利用大量烃源岩地球化学数据,从有机质丰度,有机质类型和有机成熟度三个方面分析了吐哈盆地十三尖房地区煤系烃源岩的地球化学特征。 。结果表明,研究区侏罗系西山窑组(J(2)x)厚度大,分布连续,烃源岩成熟度高,是该研究区的主要烃源岩层。将地震数据与一维和二维盆地模拟技术相结合,研究了十三尖坊地区烃源岩的分布特征。该研究区烃源岩成熟历史的模拟研究结果表明:(1)西山窑组(J(2)x)烃源岩的生烃阈值深度为1800 m,阈值温度为95摄氏度,碳氢化合物生成阈值时间约为162 Ma。 (2)西山窑组(J2x)在成油高峰期的当前地层温度为50,接近110摄氏度,Ro为0.6,接近1.1%。 (3)研究区的烃源岩成熟度显示为:西部较高,东部较低,北部较高,南部较低,有利的勘探区主要位于研究区西北。 。这项研究的结果可能对吐哈盆地小草湖凹陷边缘的油气勘探具有重要意义。

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