岩性油气藏 ›› 2024, Vol. 36 ›› Issue (4): 3543.doi: 10.12108/yxyqc.20240404
徐田录1, 吴承美1, 张金凤1, 曹爱琼2, 张腾3
XU Tianlu1, WU Chengmei1, ZHANG Jinfeng1, CAO Aiqiong2, ZHANG Teng3
摘要: 综合利用岩心、地震、测井和微地震监测等资料,在天然裂缝模型和地应力模型的约束下,运用页岩储层压裂缝网模拟研究了吉木萨尔凹陷二叠系芦草沟组天然裂缝特征及其对压裂缝网扩展的影响。研究结果表明:①吉木萨尔凹陷二叠系芦草沟组天然裂缝包括层理缝和构造缝,以层理缝为主,数量多、倾角小,裂缝数量平均为 251 条,裂缝面密度为 0.58~1.34 条/m,平均为 0.93 条/m。构造缝倾角为70°~95°,裂缝数量明显少于层理缝,根据形成时间及产状,构造缝可分为Ⅰ类和Ⅱ类构造缝。②研究区最小水平主应力为 50.41~55.22 MPa,最大水平主应力为 53.52~74.43 MPa,有利于水力压裂缝网的延伸,芦草沟组纵向存在应力隔层,最大层间应力差可达 12 MPa,水力压裂时人工裂缝不易穿层。③研究区芦草沟组页岩压裂改造以激活高角度构造缝为主,96.45% 的压裂缝为“T 形”裂缝,而“十字形”和“一字形”压裂缝仅占 2.24% 和 1.21%,芦草沟组压裂缝半缝长度为 70~100 m,高度为 10~30 m,邻近断层时由于缝长过大,易发生井窜。
中图分类号:
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