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...

阿尔金山山前带东段构造特征与油气成藏的关系

Keywords: 柴达木盆地,阿尔金山山前带,断裂体系,构造特征,油气成藏

Full-Text   Cite this paper   Add to My Lib

Abstract:

?通过对区域地质资料结合地球物理资料的综合研究表明,柴达木盆地阿尔金山山前带东段发育两组成因不同的断裂体系,分别受控于阿尔金走滑作用和东昆仑冲断作用。坪东、鄂东、牛北等主要断裂控制了“隆坡相间”的构造格局,各构造单元的形成演化差异性明显,导致了油气成藏特征的不同。早期活动的nnw向深大气源断裂控制油气富集带的形成,不同类型构造单元控制了油气藏的主要类型,晚燕山构造运动控制了油气长期运移的优势指向区和富集层系。

References

[1]  沈亚,李洪革,管俊亚等.柴西地区古近系—新近系含油凹陷构造特征与勘探领域[j].石油地球物理勘探.2012,47(增刊1):111-117??浏览[2]shenya,lihongge,guanjunyaetal.structurefeaturesandexplorationpotentialofthepaleogene-neogenedepressionsinwesternqaidambasin.ogp,2012,47(s1):111-117.[3]康南昌,覃素华,陈元忠等.阿尔金山东南缘构造特征及勘探前景[j].石油地球物理勘探.2005,40(2):233-237??浏览kangnanchang,qinsuhua,chenyuanzhongetal.structuralfeatureinsoutheastmarginofaljinmotuntainsandexploratiorprospect[j].ogp.2005,40(2):233-237??浏览[4]姚俊祥.试论阿尔金构造带中段的构造特征[j].新疆石油地质.1994,15(2):102-109yaojunxiang.ontectonicfeaturesofmiddlepartofaltyntectonicbelt.xinjiangpetroleumgeology,1994,15(2):102-109.[5]段宏亮,钟建华,马锋等.柴西阿尔金山前中、下侏罗统展布及油气勘探方向.中国石油大学学报(自然科学版),2006,30(6):13-18.duanhongliang,zhongjianhua,mafengetal.lower-middlejurassicdistributionandoil-gasexplorationdirectiononthesouthernaltyntaghinthewesternqaidamubasin.journalofchinauniversityofpetroleum(naturalscienceedition),2006,30(6):13-18.[6]刘永江,葛肖虹,叶慧文等.晚中生代以来阿尔金断裂的走滑模式.地球学报,2001,22(1):23-28.liuyongjiang,gexiaohong,yehuiwenetal.strike-slipmodelforaltyntaghfaultdevelopedsincelatemesozoic.actageoscientiasinica,2001,22(1):23-28.[7]杨藩,叶素娟,曹春潮等.新生代阿尔金断层中、东段右行走滑特征[j].地质科学.1994,29(4):346-354yangfan,yesujuan,caochunchaoetal.rightlateralcharacteristicsofthemiddleeasternsegmentofaltunfaultincenozoicera.scientiageologicasinica,1994,29(4):346-354.[8]刘永江,franzneubauer,葛肖虹等.阿尔金断裂带年代学和阿尔金山隆升[j].地质科学.2007,42(1):134-146liuyongjiang,franzneubauer,gexiaohongetal.gelchronologyofthealtunfaultzoneandrisingofthealtunmountans.chinesejournalofgeology,2007,42(1):134-146.[9]刘志宏,王芃,沙茜等.柴达木盆地阿尔金斜坡带构造特征与阿尔金断裂形成时间讨论.地质学报,2010,84(9):1275-1282.liuzhihong,wangpeng,shaqianetal.structuralfeaturesofaltynslopezoneandformationtimingofaltynfaultinqaidambasin.actageoloqicasinica,2010,84(9):1275-1282.[10]尹成明,任收麦,田丽艳.阿尔金断裂对柴达木盆地西南地区的影响.吉林大学学报(地球科学版),2011,41(3):724-734.yinchengming,renshoumai,tianliyan.effectofaltyntaghfaulttosouthwestqaidambasin.journalofjilinuniversity(earthscienceedition),2011,41(3):724-734.[11]袁四化,刘永江,葛肖虹等.青藏高原北缘的隆升时期.岩石矿物学杂志,2008,27(5):413-421.yuansihua,liuyongjiang,gexiaohongetal.upliftperiodofthenorthernmarginoftheqinghai-tibetplateau.actapetrologicaetmineralogica,2008,27(5):413-421.[12]张岳桥,陈正乐,杨农.阿尔金断裂晚新生代左旋走滑位错的地质新证据.现代地质,2001,15(1):8-12.zhangyueqiao,chenzhengle,yangnong.newgeologicalevidenceforlatecenozoicleft-lateraldisplacementalongthealtyntaghfault.geoscience,2001,15(1):8-12.
[2]  沈亚,李洪革,管俊亚等.柴西地区古近系—新近系含油凹陷构造特征与勘探领域[j].石油地球物理勘探.2012,47(增刊1):111-117??浏览
[3]  yaojunxiang.ontectonicfeaturesofmiddlepartofaltyntectonicbelt.xinjiangpetroleumgeology,1994,15(2):102-109.
[4]  段宏亮,钟建华,马锋等.柴西阿尔金山前中、下侏罗统展布及油气勘探方向.中国石油大学学报(自然科学版),2006,30(6):13-18.
[5]  刘永江,葛肖虹,叶慧文等.晚中生代以来阿尔金断裂的走滑模式.地球学报,2001,22(1):23-28.
[6]  yangfan,yesujuan,caochunchaoetal.rightlateralcharacteristicsofthemiddleeasternsegmentofaltunfaultincenozoicera.scientiageologicasinica,1994,29(4):346-354.
[7]  刘永江,franzneubauer,葛肖虹等.阿尔金断裂带年代学和阿尔金山隆升[j].地质科学.2007,42(1):134-146
[8]  liuyongjiang,franzneubauer,gexiaohongetal.gelchronologyofthealtunfaultzoneandrisingofthealtunmountans.chinesejournalofgeology,2007,42(1):134-146.
[9]  刘志宏,王芃,沙茜等.柴达木盆地阿尔金斜坡带构造特征与阿尔金断裂形成时间讨论.地质学报,2010,84(9):1275-1282.
[10]  liuzhihong,wangpeng,shaqianetal.structuralfeaturesofaltynslopezoneandformationtimingofaltynfaultinqaidambasin.actageoloqicasinica,2010,84(9):1275-1282.
[11]  尹成明,任收麦,田丽艳.阿尔金断裂对柴达木盆地西南地区的影响.吉林大学学报(地球科学版),2011,41(3):724-734.
[12]  yinchengming,renshoumai,tianliyan.effectofaltyntaghfaulttosouthwestqaidambasin.journalofjilinuniversity(earthscienceedition),2011,41(3):724-734.
[13]  袁四化,刘永江,葛肖虹等.青藏高原北缘的隆升时期.岩石矿物学杂志,2008,27(5):413-421.
[14]  yuansihua,liuyongjiang,gexiaohongetal.upliftperiodofthenorthernmarginoftheqinghai-tibetplateau.actapetrologicaetmineralogica,2008,27(5):413-421.
[15]  张岳桥,陈正乐,杨农.阿尔金断裂晚新生代左旋走滑位错的地质新证据.现代地质,2001,15(1):8-12.
[16]  zhangyueqiao,chenzhengle,yangnong.newgeologicalevidenceforlatecenozoicleft-lateraldisplacementalongthealtyntaghfault.geoscience,2001,15(1):8-12.
[17]  shenya,lihongge,guanjunyaetal.structurefeaturesandexplorationpotentialofthepaleogene-neogenedepressionsinwesternqaidambasin.ogp,2012,47(s1):111-117.
[18]  康南昌,覃素华,陈元忠等.阿尔金山东南缘构造特征及勘探前景[j].石油地球物理勘探.2005,40(2):233-237??浏览
[19]  kangnanchang,qinsuhua,chenyuanzhongetal.structuralfeatureinsoutheastmarginofaljinmotuntainsandexploratiorprospect[j].ogp.2005,40(2):233-237??浏览
[20]  姚俊祥.试论阿尔金构造带中段的构造特征[j].新疆石油地质.1994,15(2):102-109
[21]  duanhongliang,zhongjianhua,mafengetal.lower-middlejurassicdistributionandoil-gasexplorationdirectiononthesouthernaltyntaghinthewesternqaidamubasin.journalofchinauniversityofpetroleum(naturalscienceedition),2006,30(6):13-18.
[22]  liuyongjiang,gexiaohong,yehuiwenetal.strike-slipmodelforaltyntaghfaultdevelopedsincelatemesozoic.actageoscientiasinica,2001,22(1):23-28.
[23]  杨藩,叶素娟,曹春潮等.新生代阿尔金断层中、东段右行走滑特征[j].地质科学.1994,29(4):346-354

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133