首页|下寺湾桥镇-雨岔区陆相泥页岩生烃机理与生烃潜力研究

下寺湾桥镇-雨岔区陆相泥页岩生烃机理与生烃潜力研究

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为揭示鄂尔多斯盆地陆相泥页岩的生烃机理与生烃潜力,选取该盆地伊陕斜坡南部下寺湾桥镇-雨岔区进行页岩地球化学特征、生烃模拟实验、生烃机理和生烃模式等方面的研究.研究结果表明,研究区长7、长9 油层组烃源岩有机质丰度高,大多处于成熟—高成熟阶段,整体属于好烃源岩.长7 油层组样品在封闭黄金管生烃模拟实验中表现出较强的生烃能力,有机质类型、热演化程度和升温速度等因素对泥页岩的生烃能力有显著影响.通过地层埋藏演化阶段特征分析可知,研究区泥页岩的生烃过程主要发生在高成熟演化阶段.
Study on Gas Generation Mechanism and Potential of Continental Shale in Qiaozhen-Yucha of Xiasiwan Town
In order to reveal the gas generation mechanism and potential of of terrestrial shale in the Ordos Basin,Yucha area of the Xiasiwanqiao town is selected to conduct research such as shale geochemical characteristics,gas generation simulation experiments,gas generation mechanisms,and hydrocarbon generation models.The research results indicate that the organic matter abundance of the source rocks in the Chang 7 and Chang 9 oil reservoirs is high,most of which are mature-high mature stages,and they belong to good hydrocarbon source rocks on the whole.The shale of the Chang 7 oil reservoir shows strong hydrocarbon generation ability in the closed golden tube simulation experiment.Factors such as organic matter type,degree of thermal evolution,and heating rate have sig-nificant impacts on the hydrocarbon generation capacity of shale.The reason why the Yanchang Formation in the re-search area can have a high gas generation rate during the low maturity-maturity evolution stage is mainly closely related to organic matters such as terrestrial higher plants and lower organisms.Through the analysis of the charac-teristics of the strata buried evolution,the hydrocarbon generation process of the Yanchang Formation shale is main-ly in the high maturity stage.

Ordos Basincontinental mudstone and shaleevaluation of hydrocarbon source rockshydrocarbon generation mechanismpotential for hydrocarbon generation

杨连如、曹聪、王桂成、张凤博、李锦峰、鲁金风

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延长油田下寺湾采油厂,陕西 延安 716100

中国石化华东油气分公司泰州采油厂,江苏 泰州 225300

西安石油大学 地球科学与工程学院,西安 710065

西安石油大学 陕西省油气成藏地质学重点实验室,西安 710065

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鄂尔多斯盆地 陆相泥页岩 烃源岩评价 生烃机理 生烃潜力

2024

重庆科技学院学报(自然科学版)
重庆科技学院

重庆科技学院学报(自然科学版)

影响因子:0.329
ISSN:1673-1980
年,卷(期):2024.26(6)