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现代地质 ›› 2024, Vol. 38 ›› Issue (05): 1306-1324.DOI: 10.19657/j.geoscience.1000-8527.2024.079

• 沉积盆地油气勘探与关键技术 • 上一篇    下一篇

鄂尔多斯盆地西南部HQ地区长7段烃源岩地球化学特征与长8段原油来源分析

刘孝锐1(), 路俊刚1,2,3(), 谭开俊4, 廖建波4, 龙礼文4, 陈世加1,2,3, 李勇1,2,3, 肖正录1,2,3   

  1. 1.西南石油大学地球科学与技术学院,四川 成都 610500
    2.油气藏地质及开发工程全国重点实验室(西南石油大学),四川 成都 610500
    3.天然气地质四川省重点实验室,四川 成都 610500
    4.中国石油勘探开发研究院西北分院,甘肃 兰州 730020
  • 出版日期:2024-10-10 发布日期:2024-11-13
  • 通信作者: 路俊刚,男,教授,博士生导师,1980年出生,主要从事油气地球化学和非常规油气地质研究。Email: lujungang21@sohu.com
  • 作者简介:刘孝锐,男,硕士研究生,1999年出生,主要从事油气成藏和油气地球化学研究。Email: 2767326029@qq.com
  • 基金资助:
    国家自然科学基金项目(42072185)

Geochemical Characteristics and Oil Source Analysis of the Chang 7 and Chang 8 Members in the HQ Area, Southwestern Ordos Basin

LIU Xiaorui1(), LU Jungang1,2,3(), TAN Kaijun4, LIAO Jianbo4, LONG Liwen4, CHEN Shijia1,2,3, LI Yong1,2,3, XIAO Zhenglu1,2,3   

  1. 1. School of Geoscience and Technology, Southwest Petroleum University, Chengdu, Sichuan 610500, China
    2. National Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum University, Chengdu, Sichuan 610500, China
    3. Sichuan Natural Gas Geology Key Laboratories, Chengdu, Sichuan 610500, China
    4. Northwest Branch, Research Institute of Petroleum Exploration and Development, PetroChina, Lanzhou, Gansu 730020, China
  • Published:2024-10-10 Online:2024-11-13

摘要:

鄂尔多斯盆地西南部HQ地区是玉门油田的流转区块,是增储上产的重要勘探新区,受多期构造运动影响,油气来源备受争议。本文选取上三叠统延长组长7不同亚段泥页岩和长8段原油样品,采用总有机碳测定、岩石热解、显微组分、饱和烃气相色谱-质谱等实验分析方法,对选取的样品的地球化学特征进行研究,结合谱系聚类、多维标度、主成分分析进行油源对比,并从烃源岩有效性和油气成藏条件对油源对比结果进行合理性探讨。结果表明,(1)研究区东部长7段烃源岩总体为好-优质烃源岩级别,西部长7段烃源岩为中等-好烃源岩级别;东部长7段烃源岩以Ⅰ-Ⅱ1型干酪根为主,西部长7段烃源岩以Ⅱ1-Ⅱ2型干酪根为主;长7段烃源岩有机质热演化程度总体上处于成熟阶段;(2)HQ东部地区长8段原油由本地长73亚段黑色页岩供烃,西部长8段原油由本地长73亚段深灰色泥岩与东部长73亚段黑色页岩混合供烃;(3)长73亚段黑色页岩有机碳含量高,为优质排烃源岩;长73亚段深灰色泥岩有机碳含量较高,可作为有效排烃源岩。晚侏罗世为长8段油藏第I期油气成藏期,此时东部烃源岩生成的低熟油主要向着研究区西部的构造高部位运移;早白垩世末期研究区西部烃源岩达到成熟,西部烃源岩生成的原油对本地长8油藏供烃。研究成果对鄂尔多斯盆地西缘进一步油气勘探具有理论指导意义。

关键词: 化学计量学, 地球化学特征, 油源对比, 长8段原油, 长7段烃源岩, 鄂尔多斯盆地

Abstract:

The HQ area in the Southwestern Ordos Basin is a transformation block in the Yumen oilfield and a key exploration area for enhancing storage and production.Due to the influence of multi-stage tectonic movements, the source of oil and gas remains controversial.In this study, shale samples from different submembers of the Chang 7 and oil samples from the Chang 8 of the Upper Triassic were analyzed.We conducted various experimental analyses in this study, including total organic carbon analysis, rock pyrolysis, maceral analysis, and saturated hydrocarbon gas chromatography-mass spectrometry.The geochemical characteristics of these samples were studied, and the oil-source correlation was performed using pedigree clustering, multidimensional scaling, and principal component analysis.The rationality of the oil-source correlation results was evaluated based on the availability of source rocks and hydrocarbon accumulation conditions.The results show that: (1) The source rocks of the Chang 7 Member in the eastern part of the study area are generally of good to high quality, whereas those in the western part are of medium to good quality.The source rocks of the Chang 7 Member in the east are primarily composed of Type I-Ⅱ1 kerogen, while those in the west are predominantly Type Ⅱ1-Ⅱ2 kerogen.The degree of thermal evolution of organic matter in the source rocks of the Chang 7 Member is generally at a mature stage.(2) The oil in the Chang 8 Member in the east area of HQ is sourced from the local black shale in the Chang 73 submember.In the contrast, the oil in the west Chang 8 Member is a mixture of local dark gray mudstone from the Chang 73 submember and black shale from the eastern Chang 73 submember.(3) The black shale of the Chang 73 submember has a high organic carbon content, served as a high-quality source rock.Additionally, the dark gray mudstone of the Chang 73 submember, also with high organic carbon content, can be considered as an effective source rock for hydrocarbon generation.The Late Jurassic was the initial stage of hydrocarbon accumulation in the Chang-8 reservoir, during which low-maturity oil from the eastern source rocks migrated to the higher structural position in the western part of the study area.By the end of the Early Cretaceous, the western source rocks in the study area had reached maturity, and the crude oil sourced from the western source rocks supplied hydrocarbons to the local Chang 8 reservoir.This study provides valuable guidance for exploring oil and gas reservoir in the lower strata of the western margin of the Ordos Basin.

Key words: chemometrics, geochemical characteristics, oil-source correlation, Chang 8 Member oil, Chang 7 Member source rock, Ordos Basin

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