岩性油气藏 ›› 2022, Vol. 34 ›› Issue (2): 141151.doi: 10.12108/yxyqc.20220213
张梦琳1, 李郭琴1, 何嘉1, 衡德2
ZHANG Menglin1, LI Guoqin1, HE Jia1, HENG De2
摘要: 综合利用地震、钻井、测井及岩心分析化验资料,分析了四川盆地西南缘天宫堂构造奥陶系五峰组—志留系龙马溪组的构造、沉积、储层及可改造性等基本地质特征,探讨了页岩气富集主控因素及成藏模式。研究结果表明:①天宫堂构造优质页岩集中分布在五峰组—龙马溪组龙一1亚段,Ⅰ类储层主要发育于龙一11—龙一13小层,厚度为0.8~17.0 m,具典型的高TOC含量、含气性好、高脆性矿物的特征。②天宫堂构造经历了晚白垩世前快速沉降、深埋藏和大量排烃阶段,形成早期富集型超压页岩气藏;晚白垩世后经2期抬升改造,早期富集型超压页岩气藏逐步向高压—常压页岩气藏调整。③研究区保存条件受地层倾角与宫1号断层的影响,造成不同构造部位页岩气差异富集。④研究区为“早期深埋藏促富集,后期隆升调富集、保存条件控富集”的背斜构造型成藏模式,构造南西翼是下步页岩气勘探开发的潜在有利区。
中图分类号:
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