石油与天然气地质 ›› 2023, Vol. 44 ›› Issue (2): 335-349.doi: 10.11743/ogg20230207
宋兴国1,2(), 陈石1,2(), 谢舟3, 康鹏飞3, 李婷3, 杨明慧1,2, 梁鑫鑫1,2, 彭梓俊3, 史绪凯3
收稿日期:
2022-06-13
修回日期:
2022-12-16
出版日期:
2023-03-17
发布日期:
2023-03-17
通讯作者:
陈石
E-mail:alexsong1996@126.com;chenshi4714@163.com
第一作者简介:
宋兴国(1996—),男,博士研究生,油区构造。E-mail: 基金项目:
Xingguo SONG1,2(), Shi CHEN1,2(), Zhou XIE3, Pengfei KANG3, Ting LI3, Minghui YANG1,2, Xinxin LIANG1,2, Zijun PENG3, Xukai SHI3
Received:
2022-06-13
Revised:
2022-12-16
Online:
2023-03-17
Published:
2023-03-17
Contact:
Shi CHEN
E-mail:alexsong1996@126.com;chenshi4714@163.com
摘要:
富满油田东部走滑断裂是塔里木盆地奥陶系超深层碳酸盐岩油气藏勘探的重点目标。该走滑断裂活动较弱,识别解译难度较大,需要深入研究其发育、演化及控藏特征。基于富满油田最新采集的三维地震数据,选取并精细解译了3条典型主干断裂(FⅠ10,FⅠ12和FⅠ17),明确了富满油田东部走滑断裂活动特征及主要活动期次。在此基础上,结合油气性质及成藏期次,分析了断裂活动特征与油气成藏的关系,加深了对该区域断裂发育特征与油气分布规律的认识,进一步明确了断裂演化与油气成藏的耦合关系对油气性质的影响。研究表明,富满油田内走滑断裂具有垂向分层差异变形特征,可划分出4个构造变形层,由下往上分别为盐下基底构造层(T2之下)、盐构造层(T2—T3)、碳酸盐岩构造层(T3—TO3t)和碎屑岩构造层(TO3t之上)。研究区断裂活动期次整体可划分为加里东早期、加里东中期Ⅲ幕和加里东晚期—海西期3个阶段,其中加里东中期Ⅲ幕是区域内断裂主要活动阶段。结合油气性质差异、油井生产动态、断裂活动特征与油气成藏期的耦合关系认为,断裂活动影响了垂向运移通道的开启,控制了油气垂向运移;断裂持续活动时间长,使油气运移通道保持开启,有利于晚期高成熟油气的持续充注,造成断控油气藏具有油气充注强度大、成熟度高及气/油比高的特征。
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