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Citation: Wu Guoqiang, Zhang Lijuan, Yang Zhenzhou, Yuan Wenfang, Qi Chunyan, Ye Yu. Paleo-karstification of the Ordovician carbonate reservoirs and the relationship with fractures in the Halahatang area of Tarim Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2017, 39(6): 790-796. doi: 10.11781/sysydz201706790

Paleo-karstification of the Ordovician carbonate reservoirs and the relationship with fractures in the Halahatang area of Tarim Basin

doi: 10.11781/sysydz201706790
  • Received Date: 2017-08-08
  • Rev Recd Date: 2017-10-20
  • Publish Date: 2017-11-28
  • The Ordovician reservoirs in the Halahatang area of Tarim Basin are carbonate reservoirs and the storage space is karstic vugs and fractures. Types and characteristics of paleo-karstification in the Ordovician carbonate reservoirs were comprehensively analyzed by outcrop study, core observation, thin section analysis, SEM-CL spectrum and SEM-EDS analysis. Coarse-clast collapsed chaotic breccia facies, fine-clast transported chaotic breccia facies, highly disturbed strata facies and undisturbed strata facies were identified in the Xikeer outcrop by outcrop analog. Chaotic breccia related to paleo-caves was found in different formations of the Ordovician under core observation. The Ordovician reservoir experienced three types of paleo-karstification, including penecontemporaneous karstification, weathering karstification and buried karstification. Different karstic vugs demonstrated different SEM-CL spectrums. Widely developed fractures in the reservoir have a significant influence on burial karstification. On one hand, factures promoted karstification by connecting stylolite networks; on the other hand, fractures induced karstification by carrying deep hydrothermal fluids into the reservoir.

     

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    Created with Highcharts 5.0.7Chart context menuAccess Area Distribution其他: 6.8 %其他: 6.8 %其他: 0.1 %其他: 0.1 %India: 0.1 %India: 0.1 %Portugal: 1.0 %Portugal: 1.0 %[]: 0.1 %[]: 0.1 %三门峡: 0.3 %三门峡: 0.3 %上海: 0.1 %上海: 0.1 %临汾: 0.1 %临汾: 0.1 %北京: 4.2 %北京: 4.2 %台州: 0.1 %台州: 0.1 %天津: 0.3 %天津: 0.3 %平顶山: 0.1 %平顶山: 0.1 %弗吉尼亚州: 0.4 %弗吉尼亚州: 0.4 %张家口: 6.7 %张家口: 6.7 %春川: 2.1 %春川: 2.1 %晋城: 0.1 %晋城: 0.1 %杭州: 1.3 %杭州: 1.3 %林伍德: 0.1 %林伍德: 0.1 %枣庄: 0.4 %枣庄: 0.4 %武汉: 0.8 %武汉: 0.8 %济南: 0.1 %济南: 0.1 %深圳: 0.4 %深圳: 0.4 %湘潭: 0.1 %湘潭: 0.1 %湛江: 0.3 %湛江: 0.3 %漯河: 0.3 %漯河: 0.3 %盘锦: 0.1 %盘锦: 0.1 %石家庄: 0.4 %石家庄: 0.4 %芒廷维尤: 39.7 %芒廷维尤: 39.7 %芝加哥: 1.1 %芝加哥: 1.1 %莫斯科: 0.1 %莫斯科: 0.1 %西宁: 29.1 %西宁: 29.1 %贵阳: 0.1 %贵阳: 0.1 %运城: 0.3 %运城: 0.3 %遵义: 0.4 %遵义: 0.4 %邯郸: 0.1 %邯郸: 0.1 %郑州: 0.7 %郑州: 0.7 %长沙: 0.7 %长沙: 0.7 %长治: 0.1 %长治: 0.1 %青岛: 0.1 %青岛: 0.1 %其他其他IndiaPortugal[]三门峡上海临汾北京台州天津平顶山弗吉尼亚州张家口春川晋城杭州林伍德枣庄武汉济南深圳湘潭湛江漯河盘锦石家庄芒廷维尤芝加哥莫斯科西宁贵阳运城遵义邯郸郑州长沙长治青岛

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