重庆市武隆地区五峰组−龙马溪组常压页岩气勘探潜力分析

    The potential of normal-pressure shale gas exploration of the Ordovician Wufeng Formation and the Lower Silurian Longmaxi Formation in Wulong area, Chongqing

    • 摘要:
      研究目的 为查明重庆市武隆地区五峰组−龙马溪组页岩气地质特征与保存条件,分析常压页岩气勘探潜力,为武隆地区实现效益开发提供参考。
      研究方法 综合渝东南地区页岩气勘探开发前期的认识与成果,从地质认识、区域构造演化、地震精细解释等方面开展研究。
      研究结果 武隆地区奥陶系五峰组−志留系龙马溪组下部页岩层各项静态指标较优越,具有良好的页岩气勘探潜力,造成武隆地区与盆缘焦石坝、南川地区单井产能差异主要受构造作用的影响。武隆地区燕山早期和燕山中晚期以挤压应力为主,有利于页岩气储层的改造和保存,喜马拉雅期以伸展应力为主,由于地层剥蚀、断裂发育、应力释放等因素,局部页岩气保存条件变差。
      结论 武隆地区具有“深水陆棚相带控制生烃基础、构造运动期次控制页岩气保存、构造样式控制页岩气富集”的特征,武隆地区东部地堑区位于伸展构造区,断层开启导致保存条件较差,不利于页岩气的勘探开发;南部凹中隆区、中部断展褶皱区为挤压应力区,正向构造的发育有利于常压页岩气的富集和高产,为页岩气勘探开发的有利目标区。

       

      Abstract:
      Objective To clarify the geological characteristics and preservation conditions of the Ordovician Wufeng Formation and the Lower Silurian Longmaxi Formation shale gas, and to analyze the potential of the shale gas under normal pressure, this paper provides a reference for the efficient development of the Wulong area.
      Methods  Based on the knowledge and achievements of shale gas exploration and development in southeast Chongqing, the research was conducted through the aspects of geological knowledge, regional tectonic evolution and fine seismic interpretation.
      Results The static evaluation indexes are superior and have good shale gas exploration potential of the Ordovician Wufeng Formation and the Lower Silurian Longmaxi Formation in this area. The difference of single well productivity is mainly due to the influence of tectonics between Wulong, Jiaoshiba and Nanchuan area. The compressive stress of Yanshan period was dominant in Wulong area, which was conducive to the transformation and preservation of shale gas reservoirs, and the extension stress was dominant in the Himalayan period, which made local shale gas preservation conditions deteriorate due to formation denudation, fracture development, stress release and other factors.
      Conclusions The Wulong area has the characteristics of "deep−water shelf facies controlling hydrocarbon generation, tectonic movement periods controlling shale gas preservation, and tectonic styles controlling shale gas enrichment". The eastern graben is located in the extensional tectonic zone, and the fault opening leads to poor preservation conditions, which is not conducive to shale gas exploration and development. The central uplift area in the southern depression and the fault−developed fold area in the central part under compressive stress are favorable targets for shale gas exploration.

       

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