岩性油气藏 ›› 2023, Vol. 35 ›› Issue (3): 99109.doi: 10.12108/yxyqc.20230309
宋兴国1,2, 陈石1,2, 杨明慧1,2, 谢舟3, 康鹏飞3, 李婷3, 陈九洲3, 彭梓俊3
SONG Xingguo1,2, CHEN Shi1,2, YANG Minghui1,2, XIE Zhou3, KANG Pengfei3, LI Ting3, CHEN Jiuzhou3, PENG Zijun3
摘要: 利用三维地震、多层相干分析、振幅变化率、储层岩心分析及油气分布特征等资料,对塔里木盆地富满油田FⅠ16断裂的空间展布特征、活动强度及期次进行了分析,并探讨了断裂的控储控藏作用。研究结果表明:①富满油田FⅠ16断裂具有平面分段、垂向分层的特征。平面上由北往南可划分为3段,北段沿NE 10°展布,发育似马尾状构造;中段沿NE 20°展布,处于断裂走向转换部位,主要发育左阶斜列;南段沿NE 30°展布,具有强线性延伸特征,以右阶斜列为主;垂向上可划分为上寒武统底面以下的深部构造变形层和上寒武统底-奥陶系一间房组顶面浅部构造变形层,深层断裂活动较弱,分支发育较少,仅局部发育花状构造,浅层断裂活动强,花状构造普遍发育,且垂向上存在"多花叠置"及破碎带内地层同沉积的现象。②FⅠ16断裂在富满油田的活动主要发生于加里东早期和加里东中期,加里东中期为主要活动期,强度较大且具有多幕次特征;活动强度在平面上表现为"北强南弱",在垂向上表现出"浅层上拱、深层下降"的特征,浅层断裂活动更强烈。③研究区储层以断控缝洞型为主,受断裂破碎作用控制,平面上沿FⅠ16断裂带呈条带状分布,垂向上具有深浅分层叠置的特征;受中寒武统膏盐岩的分布影响,FⅠ16断裂带的油气分布具有"南油北气"的特征。
中图分类号:
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