川东北通江—马路背地区须家河组断裂结构特征与裂缝发育规律

Fault structure characteristics and fracture development patterns in Xujiahe Formation of Tongjiang-Maolubei area, northwestern Sichuan Basin

  • 摘要: 四川盆地东北部通江—马路背地区须家河组“断缝体”气藏发育多期次断裂构造,其储层主要由断裂活动形成的断层伴生缝、褶皱伴生缝与基质孔隙耦合叠加而成,构成规模化的网状缝—孔储渗系统。然而,断裂内部不同结构的储集性能及裂缝发育规律尚不明确,制约了该区油气勘探的进一步突破。综合利用地质、地球物理及成像测井等多种资料,通过岩心观察、测井解释与构造精细解释等技术手段,对通江—马路背地区须家河组断裂进行系统分类,并分析不同类型断裂的内部结构特征与裂缝发育规律。研究区须家河组断裂普遍发育,可分为通源断裂、反向改造断裂和伴生断裂3类。断裂内部结构主要包括滑动破碎带、主动盘诱导破碎带与被动盘诱导破碎带3个结构,特征各异、非均质性强,不同类型断裂及其内部结构的裂缝发育程度与储渗性能存在显著差异。反向改造断裂的主动盘诱导裂缝发育带是当前“断缝体”储层勘探的主要目标区;而通源断裂的主动盘诱导裂缝发育带、反向改造断裂的被动盘诱导裂缝发育带以及滑动破碎带,则具备进一步探索的潜力。研究为通江—马路背地区致密砂岩气藏勘探突破与“断缝体”储层理论深化提供了新的思路。

     

    Abstract: Multiple phases of fault structures are developed in the fault-fracture gas reservoirs of the Xujiahe Formation in the Tongjiang-Malubei area, northeastern Sichuan Basin. The reservoirs primarily consist of fault-associated fractures, fold-associated fractures, and matrix pores generated by fault activity, which are superimposed and coupled to form a large-scale storage and permeability system with a fracture-pore network. However, the reservoir properties and fracture development patterns of different internal fault structures remain unclear, which constrains further breakthroughs in oil and gas exploration in this area. In this study, multiple data was comprehensively utilized, including geological, geophysical, and imaging logging data. Based on core observations, well logging interpretation, and detailed structural analyses, faults in the Xujiahe Formation of the Tongjiang-Malubei area were systematically classified, and the internal structural characteristics and fracture development patterns of different types of faults were investigated. Faults in the Xujiahe Formation of the study area were widely developed and could be divided into three categories: source-connecting faults, reverse reactivated faults, and associated faults. The internal fault structures mainly include three zones: slip fracture zones, active hanging wall-induced fracture zones, and passive footwall-induced fracture zones. These zones exhibited distinct structural characteristics and strong heterogeneity. The fracture development level and storage and permeability properties of different fault types and their internal structures showed significant differences. The active hanging wall-induced fracture development zones of reverse reactivated faults were the main target areas for current fault-fracture reservoir exploration. The active hanging wall-induced fracture development zones of source-connecting faults, the passive footwall-induced fracture development zones of reverse reactivated fractures, and the slip fracture zones possessed potential for further exploration. This study provides new insights for achieving exploration breakthroughs in tight sandstone gas reservoirs and for further developing the theoretical framework of fault-fracture reservoirs in the Tongjiang-Malubei area.

     

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