中国石油勘探 ›› 2023, Vol. 28 ›› Issue (5): 28-42.DOI: 10.3969/j.issn.1672-7703.2023.05.003

• 勘探案例 • 上一篇    下一篇

塔里木盆地库车南斜坡托探1井油气勘探重大突破及意义

王清华,杨海军,蔡振忠,杨宪彰,张亮,蒋俊,周露   

  1. 中国石油塔里木油田公司
  • 出版日期:2023-09-15 发布日期:2023-09-15
  • 作者简介:王清华(1968-),男,湖北潜江人,博士,2007年毕业于浙江大学,教授级高级工程师,现主要从事塔里木盆地油气勘探研究工作。地址:新疆库尔勒市石化大道26号中国石油塔里木油田公司,邮政编码:841000。
  • 基金资助:
    中国石油天然气集团有限公司攻关性应用性科技专项“超深层碎屑岩油气规模增储上产与勘探开发技术研究”(2023ZZ14)。

Major breakthrough and significance of petroleum exploration in Well Tuotan 1 on the south slope of Kuqa Depression, Tarim Basin

Wang Qinghua, Yang Haijun, Cai Zhenzhong, Yang Xianzhang, Zhang Liang, Jiang Jun, Zhou Lu   

  1. PetroChina Tarim Oilfield Company
  • Online:2023-09-15 Published:2023-09-15

摘要: 塔里木盆地库车坳陷南部斜坡带温宿—西秋地区托探1井在寒武系潜山白云岩储层获得重大突破,对库车南斜坡迎烃面多目的层潜山勘探具有重要意义。受制于地质条件复杂,该地区的油气富集规律认识不清、地质结构落实及圈闭刻画难度大,制约了潜山油气勘探。基于构造特征、潜山地层分布、生—储—盖组合、油气输导体系及勘探实践的系统分析,探讨了潜山油气成藏新模式。温宿—西秋地区古生界构造为受前冲断裂沙井子—西秋断裂和反冲断裂乌什南断裂控制的背冲式构造,F1和F2两条次级反冲断裂使得背冲构造复杂化,形成3排古生界潜山构造,每排构造自近断层到远断层区古生界潜山地层由老变新。其中寒武系潜山地层分布范围最广、呈北东东向大面积展布,潜山储层以局限台地颗粒滩相白云岩为主,受多期构造活动、长时期暴露溶蚀叠加改造,裂缝—孔洞型白云岩优质储层规模连片发育。潜山油气藏表现为三叠系黄山街组和侏罗系恰克马克组泥岩联合供烃、裂缝—孔洞型白云岩成储、上覆古近系膏盐岩封盖的生—储—盖组合样式;成藏具有“库车油气远源供烃、不整合面输导、迎烃面构造富集”的特征,主要成藏期在喜马拉雅晚期(4—1Ma)。托探1井的成功钻探,证实了温宿—西秋地区多排多类型潜山巨大的勘探潜力,重新刻画潜山圈闭面积近840km2、石油资源量约2.0×108t、天然气资源量约590×108m3,有望成为油气增储上产新的战略接替区。

关键词: 塔里木盆地, 库车坳陷, 南部斜坡带, 寒武系, 潜山成藏模式, 重大突破

Abstract: A major breakthrough has been made in the Cambrian buried hill dolomite reservoir in Well Tuotan 1 in Wensu-Xiqiu area on the south slope of Kuqa Depression in Tarim Basin, which is of great significance to the exploration of multi-target buried hill on the hydrocarbon facing side on the south slope of Kuqa Depression. Due to the complex geological conditions, there is a lack of clear understanding on hydrocarbon enrichment law, and it is difficult to identify geological structures and characterize traps, which restrict the petroleum exploration in the buried hills in the study area. Based on the systematic analysis of structural features, stratigraphic distribution in buried hill, source rock-reservoir-cap rock assemblage, hydrocarbon transport system, and exploration practice, a new pattern of hydrocarbon accumulation in the buried hill has been established. The Paleozoic structure in Wensu-Xiqiu area is a back thrust structure controlled by the front thrust Shajingzi-Xiqiu Fault and recoil thrust Wushinan Fault, which is further complicated by two secondary back thrust faults F1 and F2, forming three rows of Paleozoic buried hill structures, with the stratigraphic age from old to new from the near fault to the far fault area in each row of structures. Among them, the Cambrian buried hill strata have the largest distribution range in a NEE direction. The buried hill reservoirs are mainly composed of dolomite of restricted platform granular beach facies, and the high-quality fractured-vuggy type dolomite reservoirs are contiguously distributed after reconstructed by multi stage tectonic activities and long-term exposure and erosion. The hydrocarbon accumulation assemblage of the buried hill oil and gas reservoirs is composed of dual hydrocarbon supply by mudstone source rocks in the Triassic Huangshanjie Formation and the Jurassic Chakmak Formation, fractured-vuggy type dolomite reservoir, and cap rock of the overlying Paleogene gypsum salt rock; The hydrocarbon accumulation is characterized by “distant hydrocarbon supply from Kuqa Depression, hydrocarbon transport by unconformity surface, and hydrocarbon enrichment in structures on the hydrocarbon facing side”, with the main hydrocarbon accumulation period in the late Himalayan (4-1Ma). The successful drilling of Well Tuotan 1 has confirmed the huge exploration potential of multi-row and multi-type buried hills in Wensu-Xiqiu area, with the re delineated buried hill trap area of 840km2, and the discovered oil resources of about 2.0×108t and natural gas resources of about 590×108m3, which is expected to be a new strategic replacement area for increasing oil and gas reserves and production.

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