新疆石油地质 ›› 2026, Vol. 47 ›› Issue (2): 163-171.doi: 10.7657/XJPG20260205

• 油气勘探 • 上一篇    下一篇

普光地区须家河组天然裂缝形成机理与控制因素

祖克威()   

  1. 中国石化 中原油田分公司 勘探开发研究院河南 濮阳 457001
  • 收稿日期:2025-02-18 修回日期:2025-05-29 出版日期:2026-04-01 发布日期:2026-04-08
  • 作者简介:祖克威(1986-),男,河南新乡人,高级工程师,博士,天然裂缝评价与储层地质力学,(Tel)18537309963(Email)317205425@qq.com
  • 基金资助:
    中国石化科技攻关项目(P24208)

Formation Mechanism and Controlling Factors of Natural Fractures in Xujiahe Formation, Puguang Area

ZU Kewei()   

  1. Research Institute of Exploration and Development, Zhongyuan Oilfield Company, Sinopec, Puyang, Henan 457001, China
  • Received:2025-02-18 Revised:2025-05-29 Online:2026-04-01 Published:2026-04-08

摘要:

四川盆地普光地区须家河组试气试采效果与天然裂缝的发育程度关系密切,为了系统研究天然裂缝的形成机理与控制因素,利用野外地质露头、岩心和成像测井资料,对普光地区须家河组天然裂缝的发育类型和参数进行统计,结合区域构造演化,分析天然裂缝的形成机理和控制因素。结果表明,普光地区须家河组天然裂缝有效程度高,发育北西—南东向和北东—南西向2组有效裂缝,北西—南东向为优势方位,以低角度—斜交缝为主,开度主要为10~20 μm,渗透率主要为10~50 mD,在储层中作为重要的渗流通道;须家河组天然裂缝主要形成于3个时期:燕山运动晚期,在北西—南东向的挤压作用下形成了近南北向和北西—南东向共轭剪切裂缝,该时期形成的天然裂缝充填程度高;喜马拉雅运动早期,北西—南东向的挤压作用形成了一系列北东—南西向天然裂缝,为有效裂缝;喜马拉雅运动晚期,北东—南西向强烈的挤压作用形成了北东—南西向和近南北向共轭剪切裂缝,以及北西—南东向的局部构造伴生裂缝。普光地区须家河组天然裂缝受构造、岩性、沉积微相和岩石力学层厚度控制,其中构造是影响研究区天然裂缝发育的主控因素。

关键词: 四川盆地, 普光地区, 三叠系, 须家河组, 天然裂缝, 形成机理, 控制因素

Abstract:

The formation test and production test in the Xujiahe formation in the Puguang area of the Sichuan Basin are closely related to the development of natural fractures. Based on field geological outcrop, core and imaging logging data, the types and parameters of natural fractures in the Xujiahe formation in the Puguang area are statistically analyzed. Combining with regional tectonic evolution, the formation mechanism and controlling factors of the natural fractures are evaluated. The results show that the natural fractures in the Xujiahe formation are highly efficient. Two groups of effective fractures in NW-SE and NE-SW trending are developed in the formation. The NW-SE fractures are predominant, and dominated by low-angle oblique fractures with the aperture of 10-20 μm and the permeability of 10-50 mD, acting as important flow pathways in the reservoir. The natural fractures in the Xujiahe formation formed in three periods: (1) the late Yanshanian, when conjugate shear fractures were formed in nearly N-S and NW-SE trending under the action of NW-SE compression and then highly filled; (2) the early Himalayan, when a series of NE-SW natural fractures were formed under the NW-SE compression, and these fractures are effective; and (3) the late Himalayan, when conjugate shear fractures in NE-SW and nearly N-S trending were formed due to the intense NE-SW compression, associated with NW-SE structural fractures locally. The natural fractures in the Xujiahe formation are controlled by structure, lithology, sedimentary microfacies, and rock mechanical layer thickness, among which structure is the dominant factor.

Key words: Sichuan Basin, Puguang area, Triassic, Xujiahe formation, natural fracture, formation mechanism, controlling factor

中图分类号: