中国石油勘探 ›› 2026, Vol. 31 ›› Issue (1): 131-145.DOI: 10.3969/j.issn.1672-7703.2026.01.010

• 石油地质 • 上一篇    下一篇

鄂尔多斯盆地北缘过渡带天然气勘探发现、成藏特征与模式

何发岐1,安川1,张威1,刘震2,3,宋到福2,3,赵振2,3   

  1. 1 中国石化华北油气分公司;2 中国石油大学( 北京) 油气资源与探测国家重点实验室;3 中国石油大学( 北京) 地球科学学院
  • 出版日期:2026-01-15 发布日期:2026-01-15
  • 作者简介:何发岐(1967-),男,陕西扶风人,博士,1990年毕业于西北大学,正高级工程师,主要从事常规及非常规油气勘探、油气地质及成藏特征研究工作。地址:河南省郑州市陇海西路199号,邮政编码:450006。
  • 基金资助:
    中国石化科技公关项目“中西部三大叠合盆地及周缘资源评价”(P23244)。

Natural Gas Exploration Discoveries, Accumulation Characteristics, and Accumulation Models in the Northern Margin Transitional Zone of the Ordos Basin

He Faqi1,An Chuan1,Zhang Wei1,Liu Zhen2,3,Song Daofu2,3,Zhao Zhen2,3   

  1. 1 Sinopec North China Oil & Gas Company;2 State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum (Beijing) ;3 College of Geosciences, China University of Petroleum (Beijing)
  • Online:2026-01-15 Published:2026-01-15

摘要: 鄂尔多斯盆地北缘过渡带杭锦旗地区天然气成藏条件复杂,勘探认识经历了由“局部构造控气”向“大型岩性圈闭控气”、由“单一低饱和度岩性气藏”向“多类型气藏有序分布与差异富集”转变。尤其是“十四五”以来,相继在新召区带、十里加汗区带以及中元古界新层系取得重要发现,形成了万亿方大气区。基于盆地北缘过渡带天然气勘探新成果,充分利用新的钻井、地震、分析化验等新资料,进一步深化天然气差异化成藏、富集规律,研究取得以下新认识:杭锦旗地区石炭- 二叠系太原组和山西组两套优质气源岩环古隆起分布,奠定了盆缘过渡带大气田形成的资源基础;太原-石盒子组近物源砂砾质辫状河心滩广覆式分布,叠加构造差异演化控制了盆缘致密-常规储层有序分布;成藏关键期断层与砂体组成的优势运移输导格架控制了天然气调整与富集;在上述成藏条件认识的基础上,综合重要气区天然气藏静态与动态成藏要素,构建了近源-中期成藏、远源-两期成藏、源内-晚期成藏及新生古储潜山成藏四类天然气动态成藏模式。上述研究成果进一步拓展并丰富了大型克拉通盆地全油气系统成藏与富集理论,对鄂尔多斯超级盆地的油气勘探具有重要的指导作用。

关键词: 鄂尔多斯盆地, 杭锦旗地区, 北缘过渡带, 上古生界, 天然气, 勘探新发现, 成藏特征与模式

Abstract: Gas accumulation conditions in the Hangjinqi area of the northern marginal transition zone of the Ordos Basin are highly complex, and exploration concepts have undergone a major evolution—from “local structural gas control” to “large-scale lithologic trap–controlled gas accumulation,” and from “single low-saturation lithologic gas reservoirs” to “ordered distribution and differential enrichment of multiple reservoir types.” In particular, since the “14th Five-Year Plan” period, significant discoveries have successively been made in the Xinzhao play, the Shilijiahan play, and a newly recognized Mesoproterozoic stratigraphic interval, leading to the formation of a trillion-cubic-meterscale gas province.Based on new exploration achievements in the northern marginal transition zone of the basin, and through comprehensive utilization of newly acquired drilling, seismic, and geochemical analytical data, this study further refines the understanding of differentiated gas accumulation and enrichment processes, yielding the following new insights: (1) two high-quality Carboniferous–Permian coal-measure source rock systems, the Taiyuan and Shanxi formations, are distributed around the paleo-uplift and constitute the fundamental resource basis for the formation of large gas fields in the basin-margin transition zone; (2) the widespread development of near-source, gravelly braided-river channel-bar sand bodies in the Taiyuan–Shihezi formations, superimposed on differential tectonic evolution, controls the ordered distribution of tight and conventional reservoirs along the basin margin; (3) an advantageous migration and transport framework composed of faults and sand bodies during key accumulation periods governs gas adjustment and enrichment; and (4) on the basis of these accumulation conditions, four dynamic gas accumulation models are established by integrating static and dynamic accumulation elements of major gas provinces, namely near-source–middle-stage accumulation, far-source–multi-stage accumulation, intra-source–late-stage accumulation, and rejuvenated paleoreservoir basement-hosted accumulation.These results further extend and enrich theories of hydrocarbon accumulation and enrichment within the total petroleum system of largecratonic basins, and provide important guidance for oil and gas exploration in the Ordos super basin.

Key words: Ordos Basin, Hangjinqi area, northern marginal transition zone, Paleozoic, natural gas, exploration discoveries, accumulation characteristics, and accumulation models

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