吉林大学学报(地球科学版) ›› 2024, Vol. 54 ›› Issue (6): 2114-2127.doi: 10.13278/j.cnki.jjuese.20240225

• 地质与资源 • 上一篇    下一篇

辽西兴城尖山白垩系义县组熔岩储层分布模式

卞海越1,唐华风 1,吴斌2,石诺2,张津铭1   

  1. 1.吉林大学地球科学学院,长春130061 
    2.中海油研究总院有限责任公司,北京100028
  • 出版日期:2024-11-26 发布日期:2024-12-24
  • 通讯作者: 唐华风(1979—),男,教授,博士生导师,主要从事火山地层和火山岩储层综合方面的研究,E-mail:tanghfhc@jlu.edu.cn
  • 作者简介:卞海越(1999—),男,硕士研究生,主要从事火山储层方面的研究,E-mail:bhy22@mails.jlu.edu.cn
  • 基金资助:
    吉林省重点研发项目(20230203107SF);国家自然科学基金重大项目(41790453)

 Distribution Model of Lava Reservoir in Cretaceous Yixian Formation of Jian-shan, Xingcheng, Western Liaoning

Bian Haiyue, Tang Huafeng, Wu Bin, Shi Nuo, Zhang Jinming   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China 
    2. CNOOC Research Institute Co.,Ltd.,Beijing 100028, China
  • Online:2024-11-26 Published:2024-12-24
  • Supported by:
    Supported by the Key Research and Development Program of Jilin Province (20230203107SF) and the National Natural Science Foundation of China (41790453)

摘要: 渤海湾盆地中生界义县组熔岩储层好,但不同相结构的熔岩储层差异大,亟需建立适用于勘探早期的岩相与储层的关系。本文以辽西兴城尖山白垩系义县组熔岩为例开展研究,利用地质调查、岩矿鉴定、主量元素分析、图像分析等方法,开展岩性岩相、储层类型和储层控制因素等综合研究。研究结果表明:根据火山岩几何外形和岩石组构,识别出侵出相水上熔岩穹丘亚相和喷溢相水上熔岩流亚相。侵出相水上熔岩穹丘亚相的储层以裂缝为主,未见气孔发育,储层品质中等,呈顶好下差、储地比低、储层层数少、分布范围小的分布模式;喷溢相水上熔岩流亚相简单熔岩流微相的储集空间以气孔杏仁为主,储层品质好,呈上好下差、储地比高、储层层数多、分布范围大的分布模式。研究区火山机构的火山口—近火山口相带熔岩穹丘和近源相带简单熔岩流受到构造作用和风化作用的改造后,熔岩穹丘物性变化大,而简单熔岩流变化不明显。综上,在火山岩勘探遇到残余熔岩类火山机构时,应将近源相带中储层物性较好的简单熔岩流作为首选目标,火山口—近火山口相带中储层物性中等的熔岩穹丘作为次要目标。


关键词: 熔岩, 火山岩储层模式, 火山机构, 义县组, 白垩系, 渤海湾盆地, 辽宁

Abstract:  There are favorable lava reservoirs in the Mesozoic Yixian Formation in the Bohai Bay basin, but lava reservoirs vary greatly in different phase structures, and there is an urgent need to establish the relationship between lithofacies and reservoirs applicable for early exploration. This study takes the lava of the Cretaceous Yixian Formation in Jianshan, Xingcheng, western Liaoning as an example. Comprehensive research on lithology, lithofacies, reservoir types, and reservoir controlling factors has been conducted using geological surveys, rock and mineral identification, major element analysis, and image analysis. The research results indicate that, based on the geometric shapes and petrofabric characteristics of volcanic rocks, the subfacies of subaqueous lava dome within the extrusive facies and the subfacies of subaqueous lava flow within the effusive facies have been identified. In the aquatic lava dome subfacies of the intrusive facies, the reservoirs are dominated by fissures, with no vesicular development, and the reservoirs are of average quality, showing a distribution pattern of good in top layers and poor in lower layers, low reserve-to-strata ratio, few reservoir layers, and limited distribution range. In the aquatic lava flow subfacies of the extrusive facies, the reservoir space of the simple lava flow microfacies is dominated by vesicular amygdale, and the reservoir is of good quality, showing a distribution pattern of good in upper layers and poor in lower layers, high reserve-to-strata ratio, a large number of reservoir layers, and large distribution range. The lava domes in the caldera-near caldera facies belt and the simple lava flows in the near-source facies belt of the volcanic edifice in the study area have been modified by tectonics and weathering. The lava domes experience great changes in physical properties, while the simple lava flows do not change significantly. In conclusion, when encountering residual lava-like volcanic edifices in volcanic exploration, simple lava flows with good reservoir properties in the near-source facies belt should be the first target, and lava domes with average reservoir properties in the caldera-near-caldera facies belt should be the secondary target.


Key words: lava, volcanic rock reservoir model, volcanic edifices, Yixian Formation, Cretaceous, Bohai Bay basin, Liaoning

中图分类号: 

  • P618.13 
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