用户名: 密码: 验证码:
海—塔盆地潜山岩石类型及分布规律研究
详细信息    本馆镜像全文|  推荐本文 |  |   获取CNKI官网全文
摘要
海-塔盆地是蒙古-大兴安岭裂谷盆地群中重要的含油气盆地之一,目前已经成为大庆油田外围盆地的勘探和开发重点地区。2001年海拉尔盆地贝尔凹陷苏德尔特潜山油藏的发现揭开了潜山勘探的序幕,使之成为实现增储上产目标的重要领域。储层是潜山成藏的关键因素之一,而正确确定岩石类型、岩相、储集空间类型、发育规律及其形成机制是储层研究的基础。目前,由于潜山储层成因的复杂性,海-塔盆地基底及潜山的基础研究甚为薄弱,岩石类型及分布规律的研究尚属空白,这严重影响了油气勘探和开发进程。本论文以取心层段岩心的详细观察与描述为基础,通过大量薄片鉴定、测井响应特征、地震反射特征及属性的分析、结合非地震资料,对海-塔盆地乌尔逊凹陷、贝尔凹陷、南贝尔凹陷和塔南凹陷的岩石类型及分布规律、“岩-电”关系、储集空间类型及影响因素进行了详细的分析研究。研究发现:(1)受晚侏罗-早白垩世蒙古-大兴安岭裂谷盆地群频繁的火山作用的影响,在海-塔盆地内形成正常陆源物质与火山喷发物质并存的相互影响、相互过渡的复杂多样的岩石类型。岩性以火山碎屑岩和火山碎屑沉积岩为主、火山熔岩和花岗岩结晶基底零星分布,并首次发现交代成因的铁白云岩。(2)通过对四个凹陷岩性的垂向、平面及剖面分布特征进行研究,认为海塔盆地基底及潜山岩石类型的分布与古地形、火山作用关系密切。(3)研究认为乌尔逊、贝尔、南贝尔凹陷潜山岩性分布具有中心式火山喷发的特征,各种岩石类型围绕火山口呈环带分布,并建立了贝尔凹陷受火山作用影响的岩相分布模式。而塔南凹陷具有裂隙式火山喷发的特征,岩浆岩沿大断裂带呈串珠状分布。(4)海-塔盆地潜山的主要储集空间类型是以裂缝为主以及与裂缝有关的孔(洞)为次而构成的孔-缝储渗系统。岩性岩相、构造及断裂作用、风化淋滤作用和流体及热液作用是影响潜山储层发育的因素,其中岩性岩相控制了原始储集条件;其它三个因素影响次生孔洞缝的发育。(5)在综合分析影响储层发育的各种因素之后,对储层条件进行分析评价,预测了四个凹陷的有利储层分布区。为成藏研究以及油气勘探奠定了坚实的基础。
The Hailar-Tamtsag Basin is one of most important basins which bearing oil and gas in the Mongolia-DaHinggan folded belts basin group, and now it has become highlight exploration and development area in periphery basins of the Daqing oil Field. The buried hill reservoir exploration has been dived on prologue and become the aim to increasing petroleum reserves, since the discovery of Sudeerte buried hill reservoir in 2001. As well as we know, reservoir is one of the key factors of buried hill hydrocarbon accumulation, and it is also the foundation of reservoir research to deal with rock-types, lithofacies, reservoir spaces type and its formation mechanism. At present, because the origin of buried hill is most complicate and the study on the rock-types and distribution in the Hailar-Tamtsag basin is also blank, that have seriously affected the process of oil or gas exploration and development. In this paper,the rock-types and distribution,“lithology-electric property”relationship, reservoir space type, characteristic and forming mechanism of buried hill reservoirs in Wuerxun, Beier, south Beier and Tamtsag South Sag depression have been researched, on the basis of the observation of drilling cores and the identification of a large number of thin slices, combining with such data as well logging, seismics and non-seismic attributes. In this paper, some important results have been obtained: (1) Impacted on the frequent volcanism in the Late Jurassic-Early Cretaceous of Mongolia-DaHinggan folded belts basin group, there are detrital material and pyroclastics simultaneously in this basin. The pyroclastic rock and clastic rock are the major type of rock, and there also exist slag and ganite. Especially, it is the first time that pearl spar was found in this area. (2) Through the analysis of the rock distribution in vertical, flat and profile, it is found that the base of Hailar-Tamuchage and buried hill types are closely related to the hypsography and volcanism. (3) It is investigated that the rock distribution is controlled by the eruption of central type in Beier sag, and the igneous-related lithofacies and distribution mode of Budate group are established. (4) The main reservoir space is a complicated reservoir and the permeation system is made up from fracture and pore, fracture is major and pore is minor which is also controlled by fracture. Tectonic and faulting, lithofacies, weather-worn and fluid is the chief four factors that affected formation of reservoir. Original accumulation types are mainly controlled by lithology and lithofacies, and secondary cavern and fracture is affected by the other three factors.(5)After the factors which affect reservoir development are analyzed comprehensively, reservoir formation condition is analyzed and favorable reservoir area in this four depressions is also predicted, that lay a foundation for reservoir play research and oil or gas exploration.
引文
[1]王青海,陈守田,唐建人.海拉尔盆地油气勘探开发前景[J].中国石油勘探,2002,7(3):16-19
    [2]侯启军.大庆探区油气勘探新进展与下步勘探方向[J].勘探战略,2004,4:1-4
    [3]冯志强,任延广,张晓东,等.海拉尔盆地油气分布规律及下步勘探方向[J].石油地质,2004,4:19-22
    [4]陈志广,张连昌,周新华,等.满洲里新右旗火山岩剖面年代学和地球化学特征[J].岩石学报,2006,22(12):2971-2986
    [5]赵澄林,二连盆地储层沉积学[M].北京石油工业出版社,1996:5,204-215
    [6]赵海玲,刘振文,李剑,等.火成岩油气储层的岩石学特征及研究方向[J].石油与天然气地质,2004,25(6):609-614
    [7]陈均亮,吴河勇,朱德丰,等.海拉尔盆地构造演化及油气勘探前景[J].地质科学,2007,42(1):147-159
    [8]张吉光,王金奎,秦龙卜,等.海拉尔盆地贝尔断陷苏德尔特变质岩潜山油藏特征[J].石油学报,2007,28(4):21-25
    [9]王玉华,张吉光,张海军.海拉尔盆地贝尔断陷布达特群变质岩储层特征及勘探方法[J].大庆石油地质与开发,2007,26(2):23-30
    [10]李春柏,张新涛,刘立,等.布达特群热流体活动及其对火山碎屑岩的改造作用—以海拉尔盆地贝尔凹陷为例[J].吉林大学学报(地球科学版),2006,36(2):221-226
    [11]张云峰,王磊,李晶.海拉尔盆地苏德尔特古潜山裂缝发育特征[J].大庆石油学院学报,2006,30(5):4-7
    [12]牛彦良,陈友福.海拉尔盆地贝尔凹陷变质岩潜山裂缝的表征方法[J].大庆石油地质与开发,2006,25(5):1-3
    [13]任丽华,林承焰,李辉等.海拉尔盆地苏德尔特构造带布达特群裂缝发育期次研究[J].吉林大学学报(地球科学版),2007,37(3):484-490
    [14]任丽华,林承焰,刘菊,等.海拉尔盆地苏德尔特构造带布达特群碎屑岩潜山油藏类型划分[J].中国石油大学学报(自然科学版),2007,31(2):9-18
    [15]陈建文,王德发,张晓东,等.松辽盆地徐家围子断陷营城组火山岩相和火山机构分析[J].地学前缘,2000,7(4):371-379
    [16]王玲,孙夕平,张研,等.松辽盆地深层断裂体系对火山岩成因和火山岩相带的控制:以徐深地区为例[J].天然气地质学,2007,18(3):389-393
    [17]陆建林,全书进,朱建辉,等.长岭断陷火山喷发类型及火山岩展布特征研究[J].石油天然气学报,2007,29(6):29-32
    [18]伍菁华,黄芸,张继武,等.火山岩相地震识别方法在准噶尔盆地东部的应用[J].天然气工业,2007,27(增刊):481-482
    [19]罗静兰,邵红梅,张成立.火山岩油气藏研究方法与勘探技术综述[J].石油学报,2003,24(1):31-38
    [20]杨辉,张研,邹才能,等.松辽盆地北部徐家围子断陷火山岩分布及天然气富集规律[J].地球物理学报,2006,49(4):1136-1143
    [21]赵建,高福红.测井资料交会图法在火山岩岩性识别中的应用[J].世界地质,2003,22(2):136-140
    [22]陈建文,魏斌,李长山,等.火山岩岩性的测井识别[J].测井技术,1997,458-459
    [23]王郑库,欧成华,李凤霞.火山岩储层岩性识别方法研究[J].国外测井技术,2007,22(1):8-11
    [24]张炯飞,权恒,武广,等.东北地区中生代火山岩形成的构造环境[J].贵金属地质,2000,9(1):33-38
    [25]吴福元,曹林.东北地区的若干重要基础地质问题[J].世界地质,18(2):1-13
    [26]冉启全,胡永乐,任宝生.火成岩岩性识别方法及其应用研究[J].中国海上油气,2005,17(1):25-30
    [27]邵正奎,孟宪禄,王洪艳,等.松辽盆地火山岩地震反射特征及其分布规律[J].长春科技大学学报,1999,29(1):33-36
    [28]邵济安,刘福田,陈辉,等.大兴安岭-燕山晚中生代岩浆活动与俯冲作用关系[J].地质学报,2001,75(1):56-62
    [29]林强,葛文春,孙德有,等.东北亚中生代火山岩的地球动力学意义[J].地球物理学报,1999,42(增刊):75-79
    [30]林强,葛文春,曹林,等.大兴安岭中生代双峰式火山岩的地球化学特征[J].地球化学,2003,32(3):208-222
    [31]吕志成,段国正,郝立波,等.满洲里-额尔古纳地区岩浆作用及其大地构造意义[J].矿物岩石,2001,21(1):77-85
    [32]吕志成,郝立波,段国正,等.满洲里-额尔古纳地区中生代火山岩地球化学研究[J].矿物学报,2000,20(4):406-414
    [33]陈志广,张连昌,周新华,等.满洲里新右旗火山岩剖面年代学和地球化学特征[J].岩石学报,2006,22(12):2971-2986
    [34]张吉光,彭苏萍,张宝玺,等.乌尔逊-贝尔断陷油气藏类型与勘探方法探讨[J].石油勘探与开发,2002,29(3):48-50.
    [35]侯启军,冯子辉,霍秋立.海拉尔盆地乌尔逊凹陷石油运移模式与成藏期[J].地球科学,2004,29(4):397-403.
    [36]黄超义,刘志宏,高军义.海拉尔盆地乌尔逊断陷构造特征和基底伸展量研究[J].世界地质,2005,24(1):48-52
    [37]张吉光,张宝玺,陈萍.海拉尔盆地苏仁诺尔成藏系统[J].石油勘探与开发,1998,1(25):25-32
    [38]刘志宏,万传彪,任延广等.海拉尔盆地乌尔逊-贝尔凹陷的地质特征及油气成藏规律[J].吉林大学学报(地球科学版),2006,36(4):527-534
    [39]赵澄林,刘孟慧,胡爱梅,等.特殊油气储层[M〕.北京石油工业出版社,1997,10-18
    [40]王华崇,冉启全,胡永乐.大港枣园油田火成岩岩相[J].石油勘探与开发,2004,31(5):21-24
    [41]罗静兰,曲志浩,孙卫,等.风化店火山岩岩相、储集性与油气的关系[J].石油学报,1996,17(1):32-38
    [42]王建国,耿师江,庞彦明,等.火山岩岩性测井识别方法以及对储层物性的控制作用[J].大庆石油地质与开发.2008,27(2):136-142
    [43]康德江,庞雄奇,张云峰.贝尔凹陷苏德尔特潜山储集性能及其主控因素[J].石油勘探与开发,2008,35(2):188-194
    [44] Atilla,Aydin.Fractures,faults,and hydrocarbon entrapment,migration and flow[J].Marine and Petroleum Geology,2000,17:797-814.
    [45] Beach A.Numerical modes of hydraulic fracturing and the syntectonic veins [J].Structual Geology,1980,2(4):425-438.
    [46] Parnell J,Honghan C,Middleton D.Significance of fibrous mineral veins in hydrocarbon migration:fluid inclusion studies[J].Journal of Geochemical Exploration , 2000 ,69-70:623-627.
    [47]王琪,史基安,薛莲花,等.碎屑储集岩成岩演化过程中流体-岩石相互作用特征—以塔里木盆地西南坳陷地区为例[J].沉积学报,1999,17(4):584-590
    [48]刘宝珺,李伟,付建奎,等.吐哈盆地地台北凹陷粘土矿物纵向异常演化与成因分析[J].地球科学-中国地质大学学报,2002,27(5):504-508
    [49]周张健.蒙脱石伊利石化的控制因素、转化机制及其转化模型的研究综述[J].地质科技情报,1994,13(4):41-46
    [50]李晓清,丘东洲,林承焰,等.车镇凹陷潜山油气藏形成条件与分布规律[M].中国石油大学出版社,2007,243-246

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700