单机斗地主手机版下载免费

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                    2. [南海海洋研究所]南海北部晚新生代火山岩浆活动的运移系统被揭示

                        JINRI,XIASHAOHONGYANJIUYUANLINGDAODEHAIYANGYANJIANGHUODONGYUDIMANDONGLIXUEXUEKETUANDUI,WEIRAONANHAIHAIDIYANJIANGHUODONGYUSHENBUDIMANJIEGOUKAIZHANXIANGXIYANJIU,JIESHILENANHAIBEIBUWANXINSHENGDAIHUOSHANYANJIANGHUODONGDEYUNYIXITONG,XIANGGUANCHENGGUOZAIGondwana Research、Earth and Planetary Science LettersHEJournal of Geophysical ResearchDENGGUOJIDIXUETOPQIKANSHANGFABIAO。

                        YANJIUXIANSHI,NANHAIBEIBULUYUANZAIZHANGLIEHEPOLIESHIQIYANJIANGSHIKUIFADE,ZHUYAOBIAOXIANWEI“PINYANJIANGXINGDALUBIANYUAN”,DANLIEHOUQIYOUQISHIHAIDIKUOZHANGTINGZHIZHIHOUQUECHANSHENGLEGUANGFANDEHUOSHANYANJIANGHUODONG,DAOZHINANHAIHAIDIHUOSHANBIANBU、LEIQIONGDIQUCHULUDAGUIMODEXUANWUYANFENBU。NANHAIBEIBUYANJIANGHUODONGRUHEYOU“PIN”DAO“FU”,ZHEIYIKEXUEWENTIJINNIANLAISHOUDAOLEGUONEIWAIHAIYANGDIZHIXUEJIAJIDAGUANZHU:HAIDIYANJIANGHUODONGQIYUANYUNALI?DIQIUSHENBUWUZHIRUHETUPOSHANGFUDICENGZULIERZUIZHONGYUNYIDAODIQIUBIAOMIAN?

                        XIASHAOHONGYANJIUYUANDENGLIYONGNANHAIBEIBUYANHAIDIQUDIZHENTAIWANGSHUJUKAIZHANLEYUANZHENCHENGXIANGYANJIU,HUODELEYANJIUQUSHENZHI1100 kmDEDIMANSUDUJIEGOU,BIAOMINGZAINANHAIBEIBUCUNZAIYITIAOQIYUANYUXIADIMANDELIANXUDISUTONGDAO,SANWEITOUSHITUQINGXIXIANSHICHUDISUTONGDAOSHIQINGXIESHANGSHENGDEMOGUTOUSHIDEDIMANZHUYANJIANGTONGDAO。YUJINGDIANLILUNRENWEIDIMANREZHUYINGSHICHUIZHIDEMINGXIANBUTONG,NANHAIDEYANJIANGTONGDAOBUJINSHIQINGXIEDE,ERQIECHENGXIANCHUCHENGCENGSHIDEBIANHUATEZHENG。JINYIBUYANJIUBIAOMING,GAIYANJIANGTONGDAOZAIDIMANZHUANHUANDAICHUJUJIBINGHENGXIANGKUOSAN,JINERXIANGSHANGFENLIECHENGDUOGEFENZHI,ZHIDAOYANSHIQUANDIBUZAICIFASHENGHUIJU,YUANZIXIADIMANDEWUZHIDEFEICHUIZHISHANGYONGZHENGSHINANHAIBEIBUYANJIANGYOU“PIN”DAO“FU”DEZHUYAOYUANYIN。(Xia et al. Teleseismic imaging of the mantle beneath southernmost China: New insights into the Hainan plume, 2016 Gondwana Research, 36:33-43.)

                      TU1. DICENGYANJIANGTONGDAO——DIMANDISUYICHANG

                      单机斗地主手机版下载免费    SHANGYONGDAOYANSHIQUANDIBUZAICIFASHENGHUIJUDEDIMANWUZHI,ZAIXIADIQIAOBIAOXIANXINGSHIDUOYANG。WANKUIYUANBOSHIDENGLIYONGHAIDIDIZHENYI(OBS)SHUJUKEHUALENANHAIBEIBUERWEIDIQIAOJIEGOU,QIJIEGUOXIANSHIXIADIQIAOCUNZAIYICHANGGAOSUTI,TONGGUODUIBILUJIAHELUPOQUZHONGCIYICHANG、GAOSUTIBOSUBI、YANSHIDIQIUHUAXUEDENGCHAYI,TICHULIANGZHEXIADIQIAOGAOSUTICUNZAIGOUZAOCHENGYINDEBUTONG,ZHENGSHIZAIYANGLUGUODUDAIZHIXIADEGAOSUTILAIZINANHAIZHANGLIEYIHOUSHENDIMANWUZHIDIQINDECHANWU,SHINANHAILIEHOUQIYANJIANGTONGDAOZAIXIADIQIAODEZHUYAOBIAOXIANXINGSHI。(Wan et al. Deep seismic structure of the northeastern South China Sea: Origin of a high-velocity layer in the lower crust, Journal of Geophysical Research: Solid Earth, 2017, doi: 10.1002/2016JB013481)。

                      单机斗地主手机版下载免费TU2. DIQIAODIBUYANJIANGTONGDAO——XIADIQIAOGAOSUTI

                      单机斗地主手机版下载免费  ZHAOFANGBOSHIDENGZONGHEYUNYONGERWEI/SANWEIDIZHENSHUJU、ZUANJINGSHUJUYIJIYANSHIXUESHUJU,JIESHILEYANJIANGTONGDAOZAISHANGDIQIAODEBIAOXIANXINGSHI。YANJIUFAXIAN,ZAINANHAIBEIBUFAXIANLEDUOQICIZHANGSHIJIANPENFADELIEHOUYANJIANGHUODONG,ZHEIXIEYANJIANGYANTIZHUYAOFAYUZAIDUANCENGZHISHANGHUOYANDUANCENGFAYU,BIAOMINGXIANCUNDEDUANCENGWEIYANJIANGPENFATIGONGLEMODUANTONGDAO,BINGYINGXIANGYANJIANGPENFADEWEIZHI,DAOZHINANHAIZHANGLIEHOUYANJIANGHUODONGPINFAN,HUOSHANFENBUGUANGFAN。(Zhao et al. Prolonged post-rift magmatism on highly extended crust of divergent continental margins (Baiyun Sag, South China Sea), Earth and Planetary Science Letters, 2016, 445:79-91.)。

                      TU3. ZUIDINGCENGDEYANJIANGTONGDAO——DUANCENG

                      单机斗地主手机版下载免费    SHANGSHUCHENGGUODEDAOLEGUOJIAZIRANKEXUEJIJINZHONGDIANXIANGMU(91328206)、YOUQINGXIANGMU(41222039)HEMIANSHANGXIANGMU(41506046)DENGDEZIZHU。TONGSHI,GANXIEGUOJIAJIJINWEIGONGXIANGHANGCIDEZHICHI。

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