岩性油气藏 ›› 2026, Vol. 38 ›› Issue (4): 126–136.doi: 10.12108/yxyqc.20260411

• 地质勘探 • 上一篇    下一篇

准噶尔盆地阜康断裂带周缘二叠纪原型盆地重建及油气勘探潜力

王彦君1,2(), 卞保力3, 向辉4, 张永军5, 孙永兴6(), 许学龙4, 马德龙1,2, 李赟7   

  1. 1 中国石油勘探开发研究院 西北分院， 兰州 730020
    2 中国石油天然气集团公司油藏描述重点实验室， 兰州 730020
    3 中国石油新疆油田公司 勘探开发研究院， 新疆 克拉玛依 834000
    4 中国石油新疆油田公司准东采油厂， 乌鲁木齐 830091
    5 中国石油集团测井有限公司 吐哈分公司， 新疆 哈密 839099
    6 乐山师范学院 旅游与地理科学学院， 四川 乐山 614000
    7 中国石油大学（北京） 克拉玛依校区， 新疆 克拉玛依 834000
  • 收稿日期:2025-12-10 修回日期:2026-03-24 出版日期:2026-07-01 发布日期:2026-07-06
  • 第一作者:王彦君（1979 —），男，博士，高级工程师，主要从事盆地构造分析和油气勘探方面的研究工作。地址：（730020）甘肃省兰州市城关区雁儿湾路535号。Email:wang_yj8@petrochina.com.cn。
  • 通信作者: 孙永兴
  • 基金资助:
    中国石油天然气股份有限公司基础性前瞻性重大科技专项“叠合盆地中下组合规模圈闭形成机制与有效性研究”(2023ZZ0205)

Reconstruction and petroleum exploration potential of the Permian prototype basin in the periphery of Fukang fault zone, Junggar Basin

WANG Yanjun1,2(), BIAN Baoli3, XIANG Hui4, ZHANG Yongjun5, SUN Yongxing6(), XU Xuelong4, MA Delong1,2, LI Yun7   

  1. 1 Research Institute of Petroleum Exploration & Development-Northwest（NWGI）, PetroChina, Lanzhou 730020, China
    2 Key Laboratory of Reservoir Discription, CNPC, Lanzhou 730020, China
    3 Research Institute of Exploration and Development, PetroChina Xinjiang Oilfield Company, Karamay 834000, Xinjiang, China
    4 Zhundong Oil Production Plant, PetroChina Xinjiang Oilfield Company, Urumqi 830091, China
    5 Tuha Branch of Logging Co., Ltd., CNPC, Hami 839099, Xinjiang, China
    6 College of Tourism and Geographical Science, Leshan Normal University, Leshan 614000, Sichuan, China
    7 China University of Petroleum-Beijing at Karamay, Karamay 834000, Xinjiang, China
  • Received:2025-12-10 Revised:2026-03-24 Online:2026-07-01 Published:2026-07-06
  • Contact: SUN Yongxing E-mail:wang_yj8@petrochina.com.cn;yohance@126.com

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摘要：

为明确阜康断裂带及周缘二叠系芦草沟组烃源岩分布范围与资源勘探潜力，综合最新地震、钻井及高精度重力资料，厘清了博格达山前地质结构与构造演化，重建了早—中二叠世盆地格局，并评估了烃源岩的资源规模。研究结果表明：①早—中二叠世，博格达及其邻区经历了由裂谷盆地到裂谷后坳陷湖盆的演化，形成“凸凹相间”的古构造格局，可划分为小泉沟凸起、阜南凹陷、吉南凸起与吉南凹陷4个二级构造单元，湖盆沉降中心位于现今博格达山以南。②自中二叠世晚期至喜山期，多期造山运动导致原湖盆中心发生构造反转与肢解，博格达山持续隆升，累计水平缩短量约62.2 km。③二叠系芦草沟组沉积期，阜康断裂带周缘发育深湖相裂谷后坳陷湖盆，原型盆地总面积约1 537 km2，其中吉南凹陷芦草沟组资源规模约为吉木萨尔凹陷的2.4倍，具备形成10.00×108 t级油页岩勘探潜力，成藏模式为“双向供烃、多层系立体成藏”，吉木萨尔与吉南凹陷作为双烃源中心，围绕石炭系火山岩古隆起风化壳、中二叠统芦草沟组页岩油及上二叠统梧桐沟组岩性-地层圈闭，形成了纵向多层叠置、横向复合连通的立体成藏体系。

关键词: 原型盆地重建, 裂谷盆地, 坳陷湖盆, 构造演化, 芦草沟组, 二叠纪, 吉木萨尔凹陷, 吉南凹陷, 阜康断裂带, 准噶尔盆地

Abstract:

To define the distribution range and resource exploration potential of Permian Lucaogou Formation source rocks in Fukang fault zone and its surrounding areas, based on the latest data of seismic, drilling, and high-precision gravity, the geological structure and tectonic evolution of Bogda piedmont were clarified. The basin configuration of Early-Middle Permian was reconstructed, and the resource scale of source rocks was assessed. Research results show that： （1） During Early-Middle Permian, Bogda and its adjacent areas underwent the evolution from a rift basin to a post-rift depression lacustrine basin, forming an paleo tectonic pattern of “alternating uplifts and sags”,which can be divided into four secondary tectonic units: Xiaoquangou uplift, Funan Sag, Jinan uplift and Jinan Sag, with the subsidence center of the lacustrine basin located south of the present-day Bogda Mountain. （2） From late Middle Permian to Himalayan period, multiple orogenic movements caused the structural inversion and dismemberment of the original lacustrine basin center,with continuous uplift of Bogda Mountain, resulting in a total horizontal shortening of about 62.2 km. （3） During the sedimentary period of Permian Lucaogou Formation, a deep lacustrine post rift depression lake basin was developed around Fukang fault zone. The total area of the prototype basin is about 153 7 km2, the resource scale of Lucaogou Formation in Jinan Sag is about 2.4 times that of Jimsar Sag, making it 10×108 ton oil shale exploration area. The reservoir formation model is “bilateral hydrocarbon supply, multi-layered stratified accumulation”. Jimsar Sag and Jinan Sag, serving as dual hydrocarbon source centers, have developed a vertically multi-stacked and laterally interconnected stratified accumulation system around Carboniferous volcanic paleo-uplifts weathered crusts, Middle Permian Lucaogou Formation shale oil, and Upper Permian Wutonggou Formation lithologic-stratigraphic traps.

Key words: prototype basin reconstruction, rift basin, depression lake basin, tectonic evolution, Lucaogou Formation, Permian, Jimsar Sag, Jinan Sag, Fukang fault zone, Junggar Basin

中图分类号: 

  • TE121.3

图1

准噶尔盆地阜康断裂带及邻区构造单元划分(a)及准噶尔盆地南缘上古生界—中生界岩性地层综合柱状图(b)"

图2

过阜康断裂带—沙奇凸起SN向地震解释（a）及地质结构剖面（b）（剖面位置见图1a）"

图3

过阜康断裂带—沙奇凸起WE向地震解释(a)及地质结构剖面（b）（剖面位置见图1a）"

图4

吉木萨尔凹陷—阜康断裂带下盘剥层剩余重力异常图（a）及构造单元解译图（b）"

图5

过阜康断裂带—吉木萨尔凹陷—沙奇凸起地震地质解释剖面（剖面位置见图1a）"

图6

过阜康断裂带—吉木萨尔凹陷—沙奇凸起剖面的构造演化恢复序列"

图7

过阜康断裂带—吉木萨尔凹陷—沙奇凸起（S—N）二叠纪原型盆地演化"

图8

准噶尔盆地东部地区中二叠世芦草沟组沉积期岩相古地理图"

图9

博格达山前油气成藏模式"

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