渤海湾盆地东营凹陷南坡东段孔二段烃源岩生排烃潜力分析
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本文为胜利石油管理局博士后科研课题“东营凹陷南坡东段孔店组油气来源与成藏过程研究”(编号:YKB2011)的成果


Hydrocarbon generation and expulsion potential of Ek2 source rocks in the southern slope of Dongying Sag
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    摘要:

    孔店组是渤海湾盆地济阳坳陷东营凹陷油气勘探向深层转移的重要层系,受演化程度较高的制约,东营凹陷南坡东段孔二段烃源岩生排烃潜能存在争议,为探讨东营凹陷深层含油气系统,明确孔二段烃源岩生排烃潜能,笔者等从含油气检测结合烃源岩分析的角度进行讨论。通过孔二段沉积时期古地貌恢复,结合地震剖面,明确了孔二段沉积时期的古地貌,探讨了孔二段烃源岩发育的平面分布特征;通过地化及薄片观察,对孔二段烃源岩有机质丰度、类型和成熟度进行研究,且对高成熟孔二段烃源岩进行原始有机碳含量恢复,结合流体包裹体测试、冷阴极发光、荧光观察等系统分析,判识孔二段烃源岩生排烃潜能。研究认为,孔二段烃源岩展布范围较大,且在沉降中心发育较厚的孔二段烃源岩层;孔二段烃源岩原始有机碳含量较高,有机质来源以高等植物为主,属于Ⅱ1-Ⅲ型有机质,成熟度较高,烃源岩已进入生气阶段,综合评定为中等—较好烃源岩。孔店组主要发生两期油充注和一期天然气充注:第一期油充注发生在沙三段沉积时期;第二期油充注发生在东营组沉积时期;第三期天然气充注发生在平原组沉积时期,结合东营凹陷古近系烃源岩生排烃模拟结果,认为孔店组原油具有孔二段烃源岩的生排烃贡献。通过分析孔二段烃源岩发育特征结合生排烃研究,判识孔二段烃源岩生排烃潜能,为东营凹陷深部含油气系统研究鉴定基础。

    Abstract:

    Currently Kongdian Formation is an important formation in the Dongying Sag, Jiyang Depression, Bohai Bay Basin, where oil and gas exploration has shifted to the deep layers. Restricted by the high degree of evolution, the hydrocarbon generation and expulsion potential of Ek2 source rocks in the eastern part of the southern slope of the Dongying sag is controversial. In order to explore the deep hydrocarbon-bearing system in the Dongying Sag and clarify the hydrocarbon generation and expulsion potential of the Ek2 source rocks , this paper discusses from the perspective of hydrocarbon-bearing detection combined with source rock analysis. Methods: Through the restoration of the paleogeomorphology during the depositional period of Ek2 Formation, combined with the seismic profile, we calrified the paleogeomorphology of the depositional period of Ek2 Formaion, and discuss the planar distribution characteristics of the Ek2 source rocks. Through geochemical analysis and thin section observation, the abundance, type and maturity of organic matter of Ek2 source rocks were studied, and the original organic carbon content of the highly mature Ek2source rocks was recovered, combined with fluid inclusion test, cold cathode luminescence, fluorescence observation on reservoir sampales of the Kongdian Formation in the east section of the south slope of Dongying Sag to identify the hydrocarbon generation and expulsion potential of the Ek2 source rocks. Results: It is believed that the Ek2 source rocks has a large distribution range, and the thicker source rock is developed in the subsidence center. The original organic carbon content of the Ek2 source rocks is relatively high, and the source of organic matter is mainly higher plants, belonging to type Ⅱ1-Ⅲ organic matter, with high maturity. The source rock has entered the gas generation stage, and is comprehensively assessed as medium-good source rocks. there are two stages of oil charging and one stage of gas charging: The first stage of oil charging occurred in the sedimentation period of the Es3 Formation; the second stage of oil charging occurred in the sedimentation period of the Dongying Formation; the third stage of gas charging occurred in the sedimentation period of the Plain Formation. Conclusions:The earliest hydrocarbon charging in Kongdian Formation occurred during the depositional period of Es3 Formation, Combined with the simulation results of hydrocarbon generation and expulsion of Paleogene source rocks in Dongying Sag, it is believed that the Ek2 source rocks gives the contribution of Kongdian Formation oil. The hydrocarbon generation and expulsion potential of Ek2 source rocks is identified by analyzing the development of Ek2 source rocks in combination with hydrocarbon generation and expulsion research, which is the basis for the research and identification of deep petroleum system in Dongying Sag.

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王玉伟,刘惠民,焦红岩,王学军,路智勇,赵海燕,刘金友,陈红汉.2022.渤海湾盆地东营凹陷南坡东段孔二段烃源岩生排烃潜力分析[J].地质论评,68(3):2022062041,[DOI].
WANG Yuwei, LIU Huimin, JIAO Hongyan, WANG Xuejun, LU Zhiyong, ZHAO Haiyan, LIU Jinyou, CHEN Honghan.2022. Hydrocarbon generation and expulsion potential of Ek2 source rocks in the southern slope of Dongying Sag[J]. Geological Review,68(3):2022062041.

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  • 收稿日期:2022-01-15
  • 最后修改日期:2022-05-10
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  • 在线发布日期: 2022-06-20
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