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    雪峰隆起西南缘寒武系乌训组页岩气成藏地质特征与资源潜力分析

    Geological characteristics and resource potential of shale gas in Cambrian Wuxun Formation in the southwestern margin of the Xuefeng uplift, China

    • 摘要:
      研究目的 2020年,雪峰隆起西南缘下寒武统乌训组首次发现页岩气显示,但其成藏条件和勘探潜力不清。
      研究方法 基于野外地质调查、钻探资料,结合有机地化分析、岩石矿物、储层物性测试等分析手段,对雪峰西南缘下寒武统乌训组页岩特征及含气性进行综合研究。
      研究结果 (1)乌训组沉积于碳酸盐岩外缓坡相,与川中龙王庙组为同时异相。(2)富有机质页岩发育在乌训组中下部,岩石组合为钙质碳质页岩夹薄层灰岩,厚度30~80 m,呈北东−南西狭长分布。(3)富有机质页岩TOC 平均为 1%,有机质类型为 I 型腐泥型,Ro平均为 2.02%,热演化程度适中。(4)页岩脆性矿物含量在43%~69%,均值为59.2%,黏土矿物含量在16%~37%,均值为28.2%,硅质含量高,脆性较大,易于储层改造。(5)页岩为超低孔超低渗储层,粘土矿物层间孔隙、溶蚀孔、粒间/晶间孔、有机质孔、为页岩气富集提供了储集空间,但至少4期构造作用造成页岩发育微裂缝大大改善了页岩储集能力。
      结论 综合页岩气形成富集及保存条件等评价指标,提出雪峰西南缘兴仁向斜东翼可作为页岩气勘探有利区。

       

      Abstract:
      This paper is the result of shale gas geological survey engineering.
      Objective  In 2020, shale gas were first discovered in the Lower Cambrian Wuxun Formation on the southwestern margin of the Xuefeng uplift, but its accumulation conditions and exploration potential are unknown.
      Methods Based on field geological survey and drilling data, combined with organic geochemical analysis, a comprehensive study of the Lower Cambrian Wuxun Formation in the southwestern margin of Xuefeng was carried out.
      Results (1) The shale of the Wuxun Formation was deposited in the outer ramp subfacies of carbonate facies, which is an different subfacies from the contemporary Longwangmiao Formation in central Sichuan. (2) The organic shale is developed in the middle and lower parts of the Wuxun Formation, and its lithological unit is calcareous carbonaceous shale intercalated with thin limestone, with a thickness of 30–80 m and a long and narrow northeast-southwest distribution. (3) The average TOC content of shale organic matter is 1%, the type of organic matter is sapropelic I-type, and the average Ro is 2.02%, reflecting a moderate-degree thermal evolution. (4) The content of brittle minerals in shale ranges from 43% to 69%, with an average value of 59.2%, and that of clay minerals ranges from 16% to 37%, with an average value of 28.2%. Therefore, the shale is charactered by high siliceous content and high brittleness, which is easy for reservoir stimulation. (5) The shale is a low-porosity and low-permeability reservoir. Organic pores, intercrystalline pores, interlayer pores, and dissolved pores of carbonate mineral provide storage space for shale-gas enrichment, but at least four-stages structural fractures and the shale cleavage domain resulted in tectonism greatly improve the shale storage capacity.
      Conclusions Comprehensive evaluation indicators such as geochemistry, reservoir physical properties and preservation conditions suggest that the eastern flank of the Xingren syncline in the southwestern margin of the Xuefeng uplift can be a favorable area for shale-gas exploration.

       

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