石油学报 ›› 2025, Vol. 46 ›› Issue (7): 1294-1307.DOI: 10.7623/syxb202507005

• 地质勘探 • 上一篇    

准噶尔盆地盆1井西凹陷湾探1井风城组油气勘探突破及意义

尤新才1, 张天环2, 朱永才1, 江梦雅1, 刘龙松1, 潘进1, 王江涛1, 苏东旭1, 陈海龙1   

  1. 1. 中国石油新疆油田分公司勘探开发研究院 新疆克拉玛依 834000;
    2. 中国石油新疆油田分公司石西油田作业区 新疆克拉玛依 834000
  • 收稿日期:2024-11-08 修回日期:2025-06-18 发布日期:2025-08-08
  • 通讯作者: 张天环,男,1995年3月生,2018年获东北石油大学学士学位,现为中国石油新疆油田分公司石西油田作业区工程师,主要从事滚动勘探与油藏评价研究。Email:sxytzth@petrochina.com.cn
  • 作者简介:尤新才,男,1982年12月生,2005年获中国石油大学(北京)学士学位,现为中国石油新疆油田分公司勘探开发研究院高级工程师,主要从事油气地质勘探研究。Email:youxc@petrochina.com.cn
  • 基金资助:
    新疆维吾尔自治区天山英才-科技创新领军人才支持项目“北疆地区二叠系超级盆地全油气系统地质理论研究与战略接替领域优选”(2022TSYCLJ0070)资助。

Hydrocarbon exploration breakthrough of Fengcheng Formation of Well WT1 in the Well Pen-1 West sag of Junggar Basin and its significance

You Xincai1, Zhang Tianhuan2, Zhu Yongcai1, Jiang Mengya1, Liu Longsong1, Pan Jin1, Wang Jiangtao1, Su Dongxu1, Chen Hailong1   

  1. 1. Research Institute of Exploration and Development, PetroChina Xinjiang Oilfield Company, Xinjiang Karamay 834000, China;
    2. Shixi Oilfield Operation Area, PetroChina Xinjiang Oilfield Company, Xinjiang Karamay 834000, China
  • Received:2024-11-08 Revised:2025-06-18 Published:2025-08-08

摘要: 准噶尔盆地盆1井西凹陷二叠系风城组是盆地天然气勘探的重点层系之一,前期的源边勘探偶有突破,但规模不大。2023年,在莫索湾凸起带部署的湾探1井(WT1井)获得高产工业气流,证实了风城组的勘探潜力,同时为寻找规模天然气接替新领域提供了依据,具有重要的理论及实践意义。为进一步扩大盆1井西凹陷的天然气勘探成果,基于高精度地震资料与多井钻探成果,开展了天然气成藏要素与成藏机制研究。研究结果表明:①盆1井西凹陷风城组源边凸起区发育风城组三段(风三段),储层岩性为砂砾岩,而源内斜坡区发育风城组二段(风二段)和风城组一段(风一段),其中,风二段以泥岩为主,为主力烃源岩层,风一段的储层为低位域砂岩及白云质砂岩;②盆1井西凹陷源内斜坡区风城组发育退积型辫状河三角洲沉积储层,发育超覆背景下的源边地层-岩性常规气藏和源内连续型致密砂岩气藏。盆1井西凹陷已将勘探战场延伸至源内斜坡区,锁定有利勘探区面积超过3 000 km2,天然气资源潜力超过4 000×108m3,有望成为准噶尔盆地天然气勘探开发的主战场之一。

关键词: 准噶尔盆地, 盆1井西凹陷, 湾探1井, 风城组, 致密砂岩气藏

Abstract: The Permian Fengcheng Formation in the Well Pen-1 West sag of Junggar Basin is one of the key strata for natural gas exploration. Previous source-proximal exploration led to occasional modest-scale breakthroughs. In 2023, the Well WT1 deployed in the Mosuwan uplift achieved high-yield industrial gas flow, thus confirming the exploration potential of Fengcheng Formation. This provides a basis for identifying new gas replacement plays, and is of great theoretical and practical significance. To further advance exploration, a study was carried out to investigate the gas accumulation elements and mechanisms using high-precision seismic data and exploration drilling results from multiple wells. The study shows as follows. (1) Glutenite reservoirs are developed in Member 3 of Fengcheng Formation in the source-proximal uplift area of the Well Pen-1 West sag. In the in-source slope area, the Member 2 and Member 1 of Fengcheng Formation are developed. The Member 2 of Fengcheng Formation is primarily composed of mudstone, as the primary hydrocarbon source rock, and the Member 1 of Fengcheng Formation is dominated by lowstand sandstone and dolomitic sandstone. (2) In the in-source slope area of the Well Pen-1 West sag, Fengcheng Formation develops retrogradational braided river delta sedimentary reservoirs, conventional stratigraphic-lithologic gas reservoirs in the source-proximal zone under the background of sedimentary overlap, and continuous tight sandstone gas reservoirs in the source rock. Exploration in the Well Pen-1 West sag has been extended into the in-source slope area, identifying a favorable exploration zone of exceeding 3 000 km2. With the natural gas resource potential exceeding 400 billion cubic meters, this area is expected to become one of the primary targets for natural gas exploration and development in Junggar Basin.

Key words: Junggar Basin, Well Pen-1 West sag, Well WT1, Fengcheng Formation, tight sandstone gas reservoir

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