
新疆石油地质 ›› 2026, Vol. 47 ›› Issue (2): 163-171.doi: 10.7657/XJPG20260205
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)基金资助: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。
中图分类号:
祖克威. 普光地区须家河组天然裂缝形成机理与控制因素[J]. 新疆石油地质, 2026, 47(2): 163-171.
ZU Kewei. Formation Mechanism and Controlling Factors of Natural Fractures in Xujiahe Formation, Puguang Area[J]. Xinjiang Petroleum Geology, 2026, 47(2): 163-171.
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