岩性油气藏 ›› 2023, Vol. 35 ›› Issue (4): 90–101.doi: 10.12108/yxyqc.20230409

• 地质勘探 • 上一篇    下一篇

准噶尔盆地阜康断裂带上盘二叠系芦草沟组页岩油地质特征及勘探潜力

刘海磊1, 朱永才1, 刘龙松1, 尹鹤1, 王学勇1, 杜小弟2   

  1. 1. 中国石油新疆油田公司 勘探开发研究院, 新疆 克拉玛依 834000;
    2. 中国地质调查局 油气资源调查中心, 北京 100029
  • 收稿日期:2022-07-29 修回日期:2022-09-06 出版日期:2023-07-01 发布日期:2023-07-01
  • 第一作者:刘海磊(1986-),男,硕士,高级工程师,主要从事油气地质勘探方面的研究工作。地址:(834000) 新疆维吾尔自治区克拉玛依市克拉玛依区准噶尔路29号勘探开发研究院。Email:lhlei66@petrochina.com.cn。
  • 基金资助:
    中国石油股份公司“十四五”重大前瞻性基础性重大科技项目“陆相深层超深层油气富集规律与勘探评价技术研究”课题6“准噶尔盆地凹陷区下组合轻质油与天然气成藏规律研究”（编号：2021DJ0206）资助。

Geological characteristics and exploration potential of shale oil of Permian Lucaogou Formation in hanging wall of Fukang fault zone， Junggar Basin

LIU Hailei1, ZHU Yongcai1, LIU Longsong1, YIN He1, WANG Xueyong1, DU Xiaodi2   

  1. 1. Research Institute of Exploration and Development, PetroChina Xinjiang Oilfield Company, Karamay 834000, Xinjiang, China;
    2. Oil & Gas Survey, China Geological Survey, Beijing 100029, China
  • Received:2022-07-29 Revised:2022-09-06 Online:2023-07-01 Published:2023-07-01

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摘要： 利用露头、岩心薄片及地球化学分析资料，对准噶尔盆地阜康断裂带上盘二叠系芦草沟组的岩性、沉积古环境、烃源岩评价及分布特征进行了研究，并探讨了成藏模式。研究结果表明： ①阜康断裂带芦草沟组发育砂岩、泥页岩、碳酸盐岩等多种岩性，以灰黑色、黑色油页岩为主，厚度为200～600 m，见碳酸盐岩与泥页岩互层，碳酸盐岩夹层中可见沥青、油迹。②研究区芦草沟组沉积时期为半深湖—深湖相，气候以干热为主，间歇性出现温湿气候，古水体为微咸水—咸水；博格达山北麓为沉积湖盆的中心，具有更好的沉积和保存条件。③研究区烃源岩有机质丰度高，野外露头岩心Ro值为0.74%～1.28%，钻井岩心TOC值为0.92%～4.48%，主要为Ⅰ和Ⅱ1型，成熟度较高，生烃潜量大，S1+S2多大于20 mg/g，为成熟优质烃源岩；博格达山北麓比西侧烃源岩发育规模更大，成熟度更高，氯仿沥青“A”含量多高于1 200×10-6。④研究区芦草沟组油藏受控于圈闭和断层，北部高陡带油藏多出露地表，遭受破坏，以稠油为主，中部鼻隆带构造稳定，发育8处圈闭；中部鼻隆带油藏表现出自生自储、多期充注的特征，区域内东南部为页岩油勘探的“甜点”区。

关键词: 烃源岩, 页岩油气, 有机质丰度, 芦草沟组, 二叠系, 阜康断裂带上盘, 准噶尔盆地

Abstract: Based on outcrops，cores and geochemistry analytical data，the lithologies，sedimentary paleoenvironment，the evaluation and distribution characteristics of source rocks of Permian Lucaogou Formation in the hanging wall of Fukang fault zone in Junggar Basin were analyzed，and the hydrocarbon accumulation model was discussed. The results show that： （1）There were sandstone，shale and carbonate rocks developed in Lucaogou Formation in Fukang fault zone，and they were dominated by gray-black and black oil shale with thickness of 200- 600 m. The carbonate rocks and shale were interbedded，and asphalt and oil traces can be seen in carbonate interbeds.（2）The Lucaogou Formation in the study area was deposited during the semi-deep lake to deep lake facies，the climate was mainly dry and hot，with intermittent warm and wet climate，and the ancient water body was brackish-saline water. The northern foot of Bogda Mountain was the center of the sedimentary lake basin， which has better deposition and preservation conditions.（3）It was a high mature and high-quality hydrocarbon source rock with abundance of organic matter in the study area，with outcrops Ro of 0.74%-1.28% and drilling core TOC of 0.92%-4.48%. They are mainly typeⅠ and Ⅱ1 and have high hydrocarbon potential，with S1+S2 greater than 20 mg/g. The hydrocarbon source rocks at the northern foot of Bogda Mountain has a larger scale of development and higher maturity than that in the western side，and the chloroform asphalt “A” content is greater than 1 200× 10-6.（4）The reservoirs of Lucaogou Formation in the study area are controlled by traps and faults. The reservoirs in the northern high steep zone are mostly exposed on the surface，damaged，and dominated by thick oil. The central nasal ridge zone is tectonically stable，with eight traps developed. The reservoirs in the central nasal ridge zone are characterized by self-generation and multi-phase filling. The southeastern part can be designated as the sweet spot area for shale oil exploration.

Key words: source rocks, shale oil and gas, organic matter abundance, Lucaogou Formation, Permian, hanging wall of Fukang fault zone, Junggar Basin

中图分类号: 

  • TE122
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