全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...

渤南洼陷沙四上亚段储层异常高孔带及优质储层成因机制

Keywords: 渤南洼陷,沙四上亚段,异常高孔带,优质储层

Full-Text   Cite this paper   Add to My Lib

Abstract:

?渤南洼陷沙四上亚段碎屑岩储层约3000~4000m的深度范围存在明显的异常高孔带。结合岩心实测物性数据,利用连续深度区间的孔隙度分布图和建立的孔隙度—深度拟合曲线确定异常高孔隙带识别标准和分布范围。综合铸体薄片数据、扫描电镜分析、地层压力数据等,从成岩溶蚀、异常高压和早期油气充注等方面阐释异常高孔带成因,并结合沉积微相、岩相和断裂发育等总结相对优质储层成因机制。研究认为储层异常高孔带的发育得益于异常高压对孔隙的保护、中成岩a期有机质低熟阶段的有机酸溶蚀增孔作用和早期烃类充注的保孔作用|异常高孔带的发育、原始沉积因素如优势沉积微相(扇三角洲前缘水下分流河道和分流河口砂坝等)和刚性颗粒(石英、长石和变质岩岩屑等)含量相对高值的中粗粒砂岩以及断裂的发育组成相对优质储层形成的主要条件。?

References

[1]  zhangyunfeng,fengyaqin,wangchunxiang.ananalysisofabnormalhighporosityzonedistributionandorigininreservoirrocksinshiwufaultdepression[j].journalofdaqingpetroleuminstitute,2008,32(6):5-8.[张云峰,冯亚琴,王春香.十屋断陷异常高孔带分布特征及成因[j].大庆石油学院学报,2008,32(6):5-8.]
[2]  caizhengqi,caikuang,xuzhiming,etal.carboniferousreservoircharacteristicsinsanchapingburiedstructureintheeastofsichuanandpridictionforfavourableexplorationarea[j].naturalgasgeoscience,2005,16(6):715-718.[蔡正旗,蔡矿,徐志明,等.川东三岔坪潜伏构造石炭系储层特征及有利区预测[j].天然气地球科学,2005,16(6):715-718.]
[3]  chenyongqiao,yuxinghe,zhouxingui,etal.researchondiageneticevolutionsuccessionandoccurrenceofsecondaryporosityoflowertertiaryindifferentstructralbeltofdongyingdepression[j].naturalgasgeoscience,2004,15(1):68-74.[陈永峤,于兴河,周新桂,等.东营凹陷各构造区带下第三系成岩演化与次生孔隙发育规律研究[j].天然气地球科学,2004,15(1):68-74.]
[4]  xuningning,qiulongwei,yangshengchao,etal.researchondiageneticevolutionoftheupperfourthmemberofshahejieformationreservoirinbonanstep-faultzone[j].journalofchinauniversityofmining&technology,2015,44(1):104-115.[徐宁宁,邱隆伟,杨生超,等.渤南断阶带沙四上亚段储层成岩演化研究[j].中国矿业大学学报,2015,44(1):104-115.]
[5]  yuanjing,zhaochenglin,zhangshanwen.geneticmodelofthedeepwatersaltlakeofthepaleogenesha4memberindongyingsag[j].actasedimentologicasinica,2000,18(1):114-118.[袁静,赵澄林,张善文.东营凹陷沙四段盐湖的深水成因模式[j].沉积学报,2000,18(1):114-118.]
[6]  hehong,caizhongdong.mechanismofsecondaryporeinshahejieformationofbanandepression[j].journalofoilandgastechnology,2005,27(5):557-559.[何宏,蔡忠东.渤南洼陷沙河街组次生孔隙形成机理分析[j].石油天然气学报,2005,27(5):557-559.]
[7]  wufuqiang,xianxuefu,lihoushu,etal.deepreservoirformingmechanismintheupperpartofthefourthmemberofshahejieformationinbonansubsagofshenglioilfield[j].actapetroleisinica,2003,24(1):44-48.[吴富强,鲜学福,李后蜀,等.胜利油区渤南洼陷沙四上亚段深部储层形成机理[j].石油学报,2003,24(1):44-48.]
[8]  wufuqiang,xianxuefu,huxue,etal.discussionontheformingmechanismofsecondarypores:takingbonansubsaginjiyangdepressionasanexample[j].petroleumgeologyandrecoveryefficiency,2003,10(1):3-5.[吴富强,鲜学福,胡雪,等.次生孔隙形成机制探讨:以渤南洼陷为例[j].油气地质与采收率,2003,10(1):3-5.]
[9]  xuxingyou,xuguosheng,qinrunsen.studyonhydrocarbonmigrationandaccumulationofmember4ofshahejieformationinbonansag,zhanhuadepression,china[j].journalofchengduuniversityoftechnology:science&technologyedition,2008,35(2):113-120.[徐兴友,徐国盛,秦润森.沾化凹陷渤南洼陷沙四段油气成藏研究[j].成都理工大学学报:自然科学版,2008,35(2):113-120.]
[10]  surdamrc,crosseylj,hagenes,etal.organic-inorganicandsandstonediagenesis[j].aapgbulletin,1989,73(1):1-23.
[11]  jiangmin.studyonorganicgeochemistryfeaturesofdeepsourcerocksindongying,zhanhuaandweibeisags[d].chengdu:chengduuniversityoftechology,2011.[姜敏.东营、潍北及沾化凹陷深层烃源岩有机地球化学特征研究[d].成都:成都理工大学,2011.]
[12]  luojinglan,liuxiaohong,lintong,etal.impactofdiagenesisandhydrocarbonemplacementonsandstonereservoirqualityoftheyanchangformation(uppertriassic)intheordosbasin[j].actageologicasinica,2006,80(5):664-673.[罗静兰,刘小洪,林潼,等.成岩作用与油气侵位对鄂尔多斯盆地延长组砂岩储层物性的影响[j].地质学报,2006,80(5):664-673.]
[13]  yanjianping,liuchiyang,mayanping.influenceofdiagenesisandhydrocarbonemplacementonthequalityofthefuyangreservoirinsongliaobasin[j].actasedimentologicasinica,2009,27(2):212-220.[闫建萍,刘池阳,马艳萍.成岩作用与油气侵位对松辽盆地齐家—古龙凹陷扶杨油层物性的影响[j].沉积学报,2009,27(2):212-220.]
[14]  maastte,jahrenj,bjφrrlykkek.diageneticcontrolsonreservoirqualityinmiddletoupperjurassicsandstonesinthesouthbjφrrlykkevikinggraben,northsea[j].aapgbulletin,2011,95(11):1883-1905.
[15]  gongxiumei,jinzhijun,zengjianhui,etal.resrvoiringcharacteristicsandmaincontrollingfactorsfordeephydrocarbonaccumulationsinbonansaginjiyangdepression[j].oil&gasgeology,2005,26(4):473-479.[宫秀梅,金之钧,曾溅辉,等.渤南洼陷深层油气成藏特征及主控因素[j].石油与天然气地质,2005,26(4):473-479.]
[16]  xiaolihua,gaoyunting,tianweizhi,etal.theretardationofmechanicalcompactioninclasticrocksbyoverpressureandthepredictionmodelforporosity[j].bulletinofmineralogy,petrologyandgeochemistry,2011,30(4):400-406.[肖丽华,高煜婷,田伟志,等.超压对碎屑岩机械压实作用的抑制与孔隙度预测[j].矿物岩石地球化学通报,2011,30(4):400-406.]
[17]  rammm,bjφrrlykkek.porosity/depthtrendsinreservoirsandstones:assessingthequantitativeeffectsofvaryingpore-pressure,temperaturehistoryandmineralogy,norwegianshelfdata[j].clayminerals,1994,29(4):475-490.
[18]  haofang,zouhuayao,nijianhua,etal.evolutionofoverpressuredsystemsinsedimentarybasinsandconditionsfordeepoil/gasaccumulation[j].earthscience:journalofchinauniversityofgeosciences,2002,27(5):610-615.[郝芳,邹华耀,倪建华,等.沉积盆地超压系统演化与深层油气成藏条件[j].地球科学:中国地质大学学报,2002,27(5):610-615.]
[19]  xiexinong,liuxiaofeng,zhaoshibao,etal.fluidflowandhydrocarbonmigrationpathwaysinabnormallypressuredenvironments[j].earthscience:journalofchinauniversityofgeosciences,2004,29(5):589-595.[解习农,刘晓峰,赵士宝,等.异常压力环境下流体活动及其油气运移主通道分析[j].地球科学:中国地质大学学报,2004,29(5):589-595.]
[20]  liuhua,jiangyoulu,guguocui,etal.pressurecharacteristicsandformationmechanismsofpaleogeneinbonansag,zhanhuadepression[j].journalofchinauniversityofpetroleum:editionofnaturalscience,2013,37(4):46-51.[刘华,蒋有录,谷国翠,等.沾化凹陷渤南洼陷古近系压力特征及成因机制[j].中国石油大学学报:自然科学版,2013,37(4):46-51.]
[21]  wangyanzhong,caoyingchang,liyongxin,etal.controllingfactorsonthepaleogenedeepeffectivereservoirsinthebonansag[j].naturalgasgeoscience,2012,23(6):996-1003.[王艳忠,操应长,李永新,等.渤南洼陷古近系深层有效储层控制因素研究[j].天然气地球科学,2012,23(6):996-1003.]
[22]  wangtianfu,caoyingchang,wangyanzhong.characteristicandoriginoftheabnormalpressureinthedeeppaleogeneformationinbonansub-sag[j].journalofxi′anshiyouuniversity:naturalscienceedition,2009,24(2):21-25.[王天福,操应长,王艳忠.渤南洼陷古近系深层异常压力特征及成因[j].西安石油大学学报:自然科学版,2009,24(2):21-25.]
[23]  qinrunsen.hydrocarbondistributionbasedonthecharacteristicsofcurrentpressurefield,es4formationinbonansag[d].chengdu:chengduuniverstyoftechology,2008.[秦润森.沾化凹陷渤南洼陷沙四段段现今压力场特征及其与油气分布关系[d].成都:成都理工大学,2008.]
[24]  wufuqiang,lihoushu,huxue,etal.anapproachtothecompositepetroleumsystemsofes41inbonansag,shenglioilprovince[j].petroleumexplorationanddevelopment,2002,29(3):29-31.[吴富强,李后蜀,胡雪,等.渤南洼陷沙四上亚段含油气系统探讨[j].石油勘探与开发,2002,29(3):29-31.]
[25]  wangduoyun,zhengximin,lifengjie,etal.formingconditionofhigh-qualityreservoiranditsrelativeproblemsinlowporosityandpermeabilityenrichmentzone[j].naturalgasgeoscience,2003,14(2):87-91.[王多云,郑希民,李风杰,等.低孔渗油气富集区优质储层形成条件及相关问题[j].天然气地球科学,2003,14(2):87-91.]
[26]  yangxiaoping,zhaowenzhi,zoucaineng,etal.originoflow-permeabilityreservoiranddistributionoffavorablereservoir[j].actapetroleisinica,2007,28(4):57-61.[杨晓萍,赵文智,邹才能,等.低渗透储层成因机理及优质储层形成与分布[j].石油学报,2007,28(4):57-61.]
[27]  zhaiyonghong,guojianhua,liushengguo,etal.studyontheorigineofqualityclasticrocksreservoirincarboniferousfromtazhongarea[j].journalofmineralogyandpetrology,1996,16(2):55-61.[翟永红,郭建华,刘生国.塔中石炭系碎屑岩深埋藏优质储层成因探讨[j].矿物岩石,1996,16(2):55-61.]
[28]  zhongdakang,zhuxiaomin,wanghongjun.characteristicandformationmechanismofdeepburiedclasticreservoir[j].scienceinchina:seriesd,2008,38(supplement1):11-18.[钟大康,朱筱敏,王红军.中国深层优质碎屑岩储层特征与形成机理分析[j].中国科学:d辑,2008,38(增刊1):11-18.]
[29]  blochs,landerrh,bonnelll.anomalouslyhighporosityandpermeabilityindeeplyburiedsandstonereservoirs:originandpredictability[j].aapgbulletin,2002,86(2):301-328.
[30]  tongchuanxin,mengyuanlin,xieyuhong,etal.distributionandcausesanalysisoftheanomalouslyhighporosityzoneoftheyinggerhaibasin[j].bulletinofmineralogy,petrologyandgeochemistry,2013,32(6):720-727.[童传新,孟元林,谢玉洪,等.莺歌海盆地异常高孔带分布与成因分析[j].矿物岩石地球化学通报,2013,32(6):720-727.]
[31]  zhangyunfeng,wangguoqiang,fubaoli,etal.thediagenesisandtheoriginofabnormalhighporosityzoneinthedeepclasticreservoirinchanglingfaultdepression[j].journalofjilinuniversity:earthscienceedition,2011,41(2):372-376.[张云峰,王国强,付宝利,等.长岭断陷深层碎屑岩储层成岩作用及异常高孔带成因[j].吉林大学学报:地球科学版,2011,41(2):372-376.]
[32]  mengyuanlin,liuwenhui,mengfanjin,etal.distributionandoriginofanomalouslyhighporosityzonesofthexujiaweizifaultdepressioninsongliaobasin[j].journalofpalaeogeography,2011,13(1):75-84.[孟元林,刘文慧,孟凡晋,等.松辽盆地徐家围子断陷深层异常高孔带分布特征与成因分析[j].古地理学报,2011,13(1):75-84.]
[33]  gutuan.characteristicsofabnormallyhighporosityzoneandfavorablereservoirfaciespredictionindeepcenozoichorizonofqingshuisag[j].naturalgasgeoscience,2008,19(3):327-333.[谷团.辽河盆地西部凹陷清水洼陷新生界深层异常高孔带特征与有利储集相预测研究[j].天然气地球科学,2008,19(3):327-333.]
[34]  wangqi,baibin,lixiaoyan,etal.diageneticevolutioncharacteristicsofdeeply-buriedclasticreserviors,northernqaidambasin:acasestudyfromwellkum2[j].naturalgasgeoscience,2008,19(2):157-164.[王琪,白斌,李小燕,等.柴达木盆地北缘深部碎屑岩储层成岩演化特征研究——以昆特依凹陷昆2井为例[j].天然气地球科学,2008,19(2):157-164.]
[35]  zhuguohua.originandevolutionandpredictionofporosityinclasticreservoirrocks[j].actasedimentologicasinica,1992,10(3):114-123.[朱国华.碎屑岩储集层孔隙的形成、演化和预测[j].沉积学报,1992,10(3):114-123.]
[36]  gujiayu,ningcongqian,jiajinhua.highqualityreservoirfeaturesandgenetieanalysisofclasticrocksinthetarimbasin[j].geologicalreview,1998,44(1):83-89.[顾家裕,宁从前,贾进华.塔里木盆地碎屑岩优质储层特征及成因分析[j].地质论评,1998,44(1):83-89.]
[37]  zhangyu.thecontrollingroleofsyndepositionalfaultstructuralslope-breakzonetodepositionalsysteminbonansub-sag[j].journalofnorthwestuniversity:naturalscienceedition,2010,41(5):860-865.[张宇.渤南洼陷同沉积断裂构造坡折带对沉积的控制作用[j].西北大学学报:自然科学版,2010,41(5):860-865.]
[38]  chenzhonghong,zhaming.mechanismofoverpressuredfluidcompartmentanditscontrollingonhydrocarbonmigrationandaccumulationinfaultedlacustrinebasin:acasestudyfromthedongyingsag,bohaibaybasin[j].chinesejournalofgeology,2008,43(1):50-64.[陈中红,查明.断陷湖盆超压封存箱形成机理与油气成藏机制——以渤海湾盆地东营凹陷为例[j].地质科学,2008,43(1):50-64.]

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133