松辽盆地南部长岭断陷青一段陆相页岩地球化学和沉积环境特征

赵晨旭; 李忠诚; 郭世超; 鲍志东; 魏兆胜; 李磊; 王海龙

doi:10.3969/j.issn.1006-6535.2023.06.008

特种油气藏 >

2023 , Vol. 30 >Issue 6: 55 - 61

DOI: https://doi.org/10.3969/j.issn.1006-6535.2023.06.008

地质勘探

松辽盆地南部长岭断陷青一段陆相页岩地球化学和沉积环境特征

赵晨旭 ,
李忠诚 ,
郭世超 ,
鲍志东 ,
魏兆胜 ,
李磊 ,
王海龙

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1.中国石油吉林油田分公司,吉林松原 138000;
2.中国石油大学(北京),北京 102249

赵晨旭(1983—),男,高级工程师,2009年毕业于西南石油大学石油工程专业,现主要从事地质勘探和钻采工程研究工作。

收稿日期: 2022-02-16

修回日期: 2023-09-28

网络出版日期: 2024-01-19

基金资助

中国石油前瞻性基础性项目“松辽盆地深部含油气系统研究”(2021DJ0205)

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Characteristics of Geochemistry and Depositional Environment of Terrestrial Shales in the First Member of Qingshankou Formation of Changling Fault Depression in the Southern Songliao Basin

Zhao Chenxu ,
Li Zhongcheng ,
Guo Shichao ,
Bao Zhidong ,
Wei Zhaosheng ,
Li Lei ,
Wang Hailong

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1. PetroChina Jilin Oilfield Company, Songyuan, Jilin 138000, China;
2. China University of Petroleum (Beijing), Beijing 102249, China

Received date: 2022-02-16

Revised date: 2023-09-28

Online published: 2024-01-19

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摘要

针对松辽盆地南部长岭断陷青一段陆相页岩地球化学和沉积环境特征认识不清的问题,系统开展有机地球化学、分子地球化学和元素地球化学实验,明确研究区陆相页岩生烃潜力,探讨沉积环境特征对有机质富集的控制作用。研究结果表明:青一段陆相页岩富含有机质,TOC平均为1.71%,氯仿沥青“A”平均为0.52%,具有良好的生烃潜力。干酪根类型主要为Ⅰ型和Ⅱ₁型,有机质热演化处于成熟阶段,热解参数T_max平均为447 ℃,R_o平均为1.06%;C₂₇—C₂₉规则甾烷指示页岩有机质主要来源于藻类等低等水生生物,兼具部分高等植物输入,微量元素比值和生物标志化合物参数指示古生产力水平较高,页岩来源于咸水—微咸水还原环境,有利于有机质保存;氯仿沥青“A”与P/Ti、Sr/Ba之比具有正相关关系,表明古生产力和保存条件共同控制页岩有机质富集。按照TOC＞2.00%、S₁＞1 mg/g的页岩油“甜点”评价标准,确定有利区面积为5 000 km²,体积法计算页岩油地质储量为54.7×10⁸t。研究结果对松辽盆地南部页岩油资源潜力评价具有战略指导意义。

关键词： 地球化学; 沉积环境; 陆相页岩油; 青一段; 长岭断陷; 松辽盆地

本文引用格式

赵晨旭 , 李忠诚 , 郭世超 , 鲍志东 , 魏兆胜 , 李磊 , 王海龙 . 松辽盆地南部长岭断陷青一段陆相页岩地球化学和沉积环境特征[J]. 特种油气藏, 2023 , 30(6) : 55 -61 . DOI: 10.3969/j.issn.1006-6535.2023.06.008

Abstract

In response to the problem of unclear understanding of geochemistry and depositional environment characteristics of terrestrial shale in the first member of Qingshankou Formation of Changling fault depression in the southern Songliao Basin, the experiments on organic geochemistry, molecular geochemistry and elemental geochemistry were systematically carried out to clarify the hydrocarbon generation potential of terrestrial shale in the study area, and to explore the controlling effect of depositional environment characteristics on the enrichment of organic matters. The study results show that the terrestrial shale in the first member of Qingshankou Formation is rich in organic matters, with an average TOC of 1.71% and an average chloroform asphalt "A" of 0.52%, which has good hydrocarbon generation potential. The types of kerogen are mainly Ⅰ and Ⅱ₁, and the thermal evolution of organic matter is at a mature stage, with the average pyrolysis parameter T_max of 447 ℃ and average R_o of 1.06%; the C₂₇-C₂₉ regular sterane indicates that the organic matter of the shale is mainly originated from lower-order aquatic organisms, such as algae, and partly imported from higher-order plants, the ratio of trace elements and biomarker compound parameters indicate that the paleoproductivity level is high, and the shale is originated from saline-water and brackish-water reducing environment, which is favorable for organic matter preservation; the chloroform asphalt "A" has a positive correlation with P/Ti and Sr/Ba, which suggests that the paleoproductivity and the preservation conditions jointly control the organic matter enrichment of shale. According to the evaluation criteria of shale oil "sweet spot" of TOC>2.00% and S₁>1 mg/g, the favorable area is determined to be 5 000 km², and the geological reserves calculated by volumetric method is 54.7×10⁸t. The study is of strategic significance for the evaluation of shale oil resource potential in the southern Songliao Basin.

Key words： geochemistry; depositional environment; terrestrial shale oil; first member of Qingshankou Formation; Changling Fault Depression; Songliao Basin

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