引文
[1] 郝天珧,SuhMancheol,王谦身等.根据重力数据研究黄海周边断裂带在海区的延伸.地球物理学报,2001,45(3):385~397HAOTianyao,SuhMancheol,WANGQianshenetal.ThestudyofextensionoffaultsinYellowSeaandadjacentregionfromgravitydata.ChineseJ.Geophys.,2002,45(3):385~397
[2] 郝天珧,SuhMancheol,阎晓蔚等.黄海中央断裂带的地球物理证据及其与边缘海演化的关系.地球物理学报,2002,46(2):179~184HAOTianyao,SuhMancheol,YANXiaoweietal.Geophysicalevi dencesforthecenterfaultinYellowSeaandtheirrelationshipwithev olutionofmarginalseas.ChineseJ .Geophys,2002,46(2):179~184
[3] 刘光鼎.中国海区及邻域地球物理场特征.北京:科学出版社,1992LIUGuangding.GeophysicalFieldFeaturesofChinaSeaandAdja centRegions.Beijing:SciencePress.1992
[4] 张文佑主编.中国海区及邻域海陆大地构造.北京:科学出版社,1986.575ZHANGWenyoued.MarineandContinentalTectonicsinChinaSeasandAdjacentRegions.Beijing:SciencePress,1986.575
[5] 金翔龙.北黄海的构造轮廓.见:金翔龙主编,黄东海地质.北京:科学出版社,1982.23~29JINXianglong.TectonicoutlineofnorthernYellowSea.In:JinXian glonged,GeologyofEastChinaSeaandYellowSea.Beijing:Sci encePress,1982.23~29
[6] 杨志坚.胶东地块构造演化及其东延去向问题.海洋地质与第四纪地质,1989,9(2):1~11YANGZhiJian.OnthetectonicevolutionofJiaodongmassifanditsextensiontoeast.MarineGeology&QuaternaryGeology,1989,9(2):1~11
[7] YinA ,NieSAn.IndentationmodeforthenorthandSouthChinacol lisionandthedevelomentoftheTan luandHonamfaultsystems,easternAsia.Tectonics,1993,12:801~813
[8] 蔡 峰.北黄海盆地基底地质特征.海洋地质动态,1996,100(169):1~3CAIFeng.GeologicalfeatureofthebasementintheNorthYellowSeabasin.MarineGeologyLetters,1996,100(169):1~3.
[9] 秦蕴珊,赵一阳,陈丽蓉等主编.黄海地质.北京:海洋出版社,1989QINYunshan,ZHAOYiyang,CHENLirong,etal.GeologyofYel lowSea.Beijing:ChinaOceanPress,1989
[10] 刘光鼎主编.中国海区及邻域地质地球物理场系列图.北京:科学出版社,1992LIUGuangdinged.GeophysicalSeriesMapsinChinaSeaandAdja centRegions.Beijing:SciencePress,1992
[11] 郝天珧,刘伊克,徐万哲.黄海和邻区重磁场及区域构造特征.地球物理学进展,1998,13(1):27~39HAOTianyao,LIUYike,SUHMancheol.GravityandmagneticfieldfeaturesandtectonicscharacteristicsinYellowSeaandadjacentre gion.ProgressinGeophysics,1998,13(1):27~39
[12] 刘福田,李强,吴华等.用于速度图像重建的层析成像法.地球物理学报,1989,32(1):46~61LIUFutian,LIQiang,WUHuaetal.OntheTomographicInverseMethodUsedinVelocityImageRecomstruction.ChineseJ.Geophys.(ActaGeophysicaSinica),1989,32(1):61~80
[13] 江为为.调和系数法与重力资料反演地壳构造.科技大学研究生院学报,1989,6(1):96~104JIANGWeiwei.Theharmoniousseriesandgravitationaldatausedtoinversecrustalstructure.JournalofGraduateSchool,USTC .19896(1):96~104
[14] 徐佩芬.大别-苏鲁造山带与华北陆块东部岩石层三维速度结构[博士论文].北京:中国科学院地质与地球物理研究所,2001.XUPeifen.SeismictomographybeneaththeDabieSulucollisionoro genanditsimplicationstotheformationandexhumationoftheultra highpressuremetamorphicrocks[Ph.D .Dissertation].Beijing:In stituteofGeologyandGeophysics,CAS .2001
[15] 龙汉春.试论华北地区地壳拉张,挤压与裂谷推服构造的成因联系.地质论评.1988.34(2):105~113LONGHanchun.RelationsofcrustalextensionandcompressiontoriftandnappestructuresinNorthChina.GeologicalReview,1988.34(2):105~113
[16] 吴根耀,陈焕疆,马 力等.苏皖地块—特提斯演化阶段独立的构造单元.古地理学报,2002,4(2):77~87WUGenyao,CHENHuanjiang,MALietal.SuWanblock:aninde pendenttectonicunitduringperiodofTethyanevolution.JournalofPalaeogeography,2002,4(2):77~87
[17] CONGBolin,ZHAIMingguo,DENNISA .Carswelletal.Petrogene sisofultrahigh pressurerocksandtheircountryrockatShuangheinDabieshan,centralChina.Eur.J .Mineral,1995,7:119~138
[18] WANGQingchen,AKIRAISHIWATARI,ZHAOZhongyanetal.Coesite bearinggranuliteretrogradedfromeclogiteinWeihai,easternChina.Eur.J .Mineral.,1993,5:141~152
[19] ZHAIMingguo,CONGBolin,GUOJinghuietal.SmNdgeochronolo gyandPetrographyofgarnetPyroxeneGranulitesintheNorthernSuluregionofChinaandtheirGeotectonicimplication.Lithos,1997,52:23~33
[20] 袁学诚,徐明才,唐文榜等.东秦岭陆壳反射地震剖面.地球物理学报,1994,37(6):749~758YUANXuecheng,XUMingcai,TANGWenbangetal.EasternQin lingseismicreflectionprofiling.C