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顺北1号走滑断裂带分段差异活动特征及其控藏效应

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塔里木盆地塔中北坡众多大型走滑断裂带是近年油气勘探开发的重点,文中通过对顺北1号走滑断裂带三维地震资料精细解释,综合前人研究成果及油气勘探实践,探讨了顺北1号走滑断裂带的差异活动特征及其控藏效应.研究表明:1)顺北1号走滑断裂带主要发育于下古生界,为一条大型左行走滑断裂带,平面展布具有分层差异性,在下古生界为线性展布,在上古生界呈雁列式展布.2)顺北1号走滑断裂带分段差异活动特征明显,研究区内可划分出张扭、压扭和纯走滑等3类12段.3)顺北1号走滑断裂带经历了多期构造演化,其中,加里东中期Ⅰ幕、加里东中期Ⅲ幕、加里东晚期—海西早期为顺北1号走滑断裂带的关键活动时期,此后的深埋阶段构造相对稳定,断裂活动微弱.4)顺北1号走滑断裂带沟通了寒武系优质烃源岩与奥陶系有利储集体,断裂带的分段差异活动造成了不同断裂段的断溶体发育程度的差异及油藏规模的差异.实钻数据表明,张扭段和压扭段油气富集程度高,纯走滑段较低.此外,主断裂与分支断裂交叉处通常高产,推测分支断裂规模及活动强弱控制了其油气富集程度.
Characteristics of segmented differential activity of Shunbei No.1 strike-slip fault zone and its effect on reservoir control
In recent years,many large strike-slip fault zones on the north slope of Tazhong have become the focus of oil and gas exploration and development in Tarim Basin.Based on the detailed interpretation of 3D seismic data of Shunbei No.1 strike-slip fault zone,the paper discusses the differential activity characteristics and reservoir control effects of Shunbei No.1 strike-slip fault zone by combining previous research results and oil and gas exploration practice.The study shows that:(1)Shunbei No.1 strike-slip fault zone mainly develops in the Lower Paleozoic and is a large left-strike-slip fault zone with stratified plane distribution,presenting linear distribution in the lower Paleozoic and en echelon distribution in the upper Paleozoic.(2)Shunbei No.1 strike-slip fault zone has obvious segmented differential activity characteristics,and the study area can be divided into three types of 12 segments,such as tension-torsion,compression-torsion and pure strike-slip.(3)The Shunbei No.1 strike-slip fault zone has undergone multiple stages of tectonic evolution,among which,the middle Caledonian Ⅰ,middle Caledonian Ⅲ,late Caledonian to early Hercynian are the key active periods of Shunbei No.1 strike-slip fault zone,and then the deep buried stage is relatively stable with weak fault activity.(4)The Shunbei No.1 strike-slip fault zone connects the Cambrian high quality source rock with favorable reservoir of Ordovician.The segmented differential activities of the fault zone result in significant differences in the development degree of fault-karst bodies and reservoir scale in different fault segments.The drilling data indicate that the degree of oil and gas enrichment is high in tensional-torsional and compressive-torsional segments,but relatively low in the pure strike-slip segment.In addition,the intersection of main fault and branch fault usually has high yield,which suggests that the scale and activity of branch fault control the degree of oil and gas enrichment.

differential activityreservoir control effectShunbei areaShunbei No.1 strike-slip fault zoneTarim Basin

古再丽努尔·艾尔肯、曹自成、耿锋、骆福嵩、唐大卿、伍亮、王玮龙

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中国地质大学(武汉)资源学院,湖北武汉 430074

中国石化西北油田分公司勘探开发研究院,新疆乌鲁木齐 830011

中国地质大学(武汉)构造与油气资源教育部重点实验室,湖北武汉 430074

差异活动 控藏效应 顺北地区 顺北1号走滑断裂带 塔里木盆地

新疆维吾尔自治区重大科技专项国家科技重大专项国家自然科学基金项目

2022A0300933550000-19-ZC0613-006342372158

2024

断块油气田
中原石油勘探局

断块油气田

CSTPCD北大核心
影响因子:1.493
ISSN:1005-8907
年,卷(期):2024.31(4)