中国石油勘探 ›› 2022, Vol. 27 ›› Issue (5): 96-105.DOI: 10.3969/j.issn.1672-7703.2022.05.009

• 石油地质 • 上一篇    下一篇

西昌盆地上奥陶统五峰组—下志留统龙马溪组优质页岩层序沉积特征及页岩气聚集模式

何伟1,2,牟必鑫1,2,陈杨1,2,李桃1,2,魏洪刚1,2,雷玉雪1,2,于璐1,2,董雪洁1,2   

  1. 1 四川省煤田地质工程勘察设计研究院;2 页岩气评价与开采四川省重点实验室
  • 出版日期:2022-09-15 发布日期:2022-09-15
  • 作者简介:何伟(1987-),男,四川广元人,硕士,2014年毕业于中国地质大学(北京),高级工程师,现主要从事非常规油气勘探与资源评价方面的研究工作。地址:四川省成都市青华路39号四川省煤田地质工程勘察设计研究院,邮政编码:610072。
  • 基金资助:
    四川省科技基金项目“西昌盆地构造特征及页岩气保存条件研究”(2018JY0625);四川省自然资源厅项目“西昌盆地页岩气资源调查评价和区块优选”(DK-2017-F-008)。

Sedimentary sequence characteristics and shale gas accumulation pattern of high-quality shale in the Upper Ordovician Wufeng Formation-Lower Silurian Longmaxi Formation, Xichang Basin

He Wei1,2,Mu Bixin1,2,Chen Yang1,2,Li Tao1,2,Wei Honggang1,2,Lei Yuxue1,2,Yu Lu1,2,Dong Xuejie1,2   

  1. 1 Sichuan Institute of Coal Field Geological Engineering Exploration and Designing; 2 Key Laboratory of Shale Gas Evaluation and Production, Sichuan Province
  • Online:2022-09-15 Published:2022-09-15

摘要: 西昌盆地多口钻井于上奥陶统五峰组—下志留统龙马溪组获得页岩气显示,其中,五峰组—龙马溪组一段(龙一段)的含气量较好,表明该层段具有良好的页岩气勘探开发潜力。为进一步做好西昌盆地龙一段的前期评价工作,综合利用岩心观察、岩心样品薄片等资料,结合测井解释,对优质页岩进行划分并对优质页岩的地层层序、沉积相、沉积模式等进行了研究。结果表明:(1)西昌盆地五峰组—龙马溪组优质页岩为①—⑤小层;(2)优质页岩可划分为两个三级层序,SQ1发育潮坪相中的生屑滩微相及深水陆棚相中的硅质泥棚微相,SQ2发育深水陆棚相中的灰质泥棚和含灰粉砂质泥棚;(3)五峰组—龙一1亚段为深水陆棚沉积,该沉积环境控制了优质页岩的发育,优质页岩有机碳含量高、硅质含量高、富含笔石;(4)断裂带发育程度、优质页岩埋深、优质页岩距断裂带的远近是影响西昌盆地五峰组—龙马溪组优质页岩层段页岩气聚集的关键因素。

关键词: 西昌盆地, 五峰组—龙马溪组, 优质页岩, 地层层序, 沉积相, 沉积模式, 页岩气聚集模式

Abstract: Shale gas shows have been observed from the Upper Ordovician Wufeng Formation-Lower Silurian Longmaxi Formation in several wells in Xichang Basin. The drilling results indicate that gas content of Wufeng Formation-first member of Longmaxi Formation (Long 1 member) is relatively good, showing promising potential for shale gas exploration and development. By comprehensively applying core observation and thin section data, and integrating with logging interpretation, the high-quality shale is classified and the stratigraphic sequence,sedimentary facies and depositional pattern are studied, so as to primarily evaluate shale gas potential of Long 1 member in Xichang Basin.The study results show that: (1) The high-quality shale of Wufeng-Longmaxi Formation is composed of five thin layers ① - ⑤ ; (2) The highquality shale is divided into two third order sequences. Deposits of bioclastic beach microfacies of tidal flat facies and siliceous mud shelf microfacies of deep-water shelf facies were developed in SQ1, while SQ2 was composed of lime mud shelf and limy sandy mud shelf deposits of deep-water shelf facies; (3) The development of high-quality shale was controlled by the deep-water shelf environment during the deposition period of Wufeng-first sub member of the first member of Longmaxi Formation (Long 11 sub member), which had high organic carbon content,high silica content and rich graptolite; (4) The shale gas accumulation in high-quality shale of Wufeng-Longmaxi Formation is affected by three key factors, i.e., development degree of fault zone, burial depth of high-quality shale and distance between the high-quality shale to fault zone.

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