冲绳海槽中部热液区及典型喷口区地形地貌特征     

郑翔  阎军  张鑫  栾振东  陈长安 《海洋地质前沿》2015,31(3)

利用最新测量的高精度深水多波束资料,对冲绳海槽中部热液活动区的地形地貌特征进行了系统的分析后发现,研究区地形情况相当复杂,起伏变化较大,总体上呈沿SW—NE向延伸的裂谷地势,裂谷水深范围约在1 500~1 800m,大量呈SW—NE向的线性海山链和裂谷、洼地地貌交错出现,分析认为其形成可能与冲绳海槽的弧后扩张作用有关。另外,通过ROV(Remotely Operated Vehicle)上获得的影像,结合浅表层沉积物和岩石样品分析发现,2处喷口地形地貌情况明显不同,Iheya North喷口区地形起伏变化大,具有较多烟囱体、丘体,周围沉积物以硫化物砂为主;Iheya Ridge则以裂隙式溢流为主,分布范围广,地形倾斜平整,少见烟囱体、丘体,底质较硬,热液沉积物分布较少。  相似文献   

Tensile stiffness analysis on ocean dynamic power umbilical   总被引：1，自引：0，他引：1  

汤明刚  阎军  王野  岳前进 《中国海洋工程》2014,28(2):259-270

Tensile stiffness of ocean dynamic power umbilical is an important design parameter for functional implementation and structural safety. A column with radial stiffness which is wound by helical steel wires is constructed to predict the tensile stiffness value of umbilicals in the paper. The relationship between the tension and axial deformation is expressed analytically so the radial contraction of the column is achieved in the relationship by use of a simple finite element method. With an agreement between the theoretical prediction and the tension test results, the method is proved to be simple and efficient for the estimation of tensile stiffness of the ocean dynamic power umbilical.  相似文献   

扬子浅滩东南海域海底潮流沙脊、沙波特征   总被引：1，自引：0，他引：1  

庄丽华  阎军  徐涛  栾振东 《海洋科学》2017,41(1):11-17

利用seabat8101多波束系统对扬子浅滩东南海底地形进行了高精度探测。发现海底呈明显近乎平行排列的条带状起伏,脊谷相间,沙脊大部分呈NW-SE向排列,发育在45~50 m水深范围之内,沙脊横剖面不对称,大部分沙脊西南侧坡度大、东北坡缓。沙脊规模略有差异,沙脊宽度约0.6~9.8 km,沙脊之间间距可达8.9~22.4 km,高度约1.8~13.3 m,研究区内最长可达53 km。部分脊槽过渡区域发育成片链状海底沙波,沙波大致呈NE-SW走向,波高约0.3~1 m,波长1 km左右。研究区中西部有海底礁石孤立地突兀于相对平坦的海底之上,暂定名为扬礁,最浅水深35.9 m,位于30°59'7.4'~31°N,124°36'48.7'~124°37'40'E。扬子浅滩东南海域沙脊是介于活动沙脊和衰亡沙脊之间的准活动沙脊。该研究将为我国海洋开发和海洋经济发展、海洋行政管理以及海洋安全保障提供服务。  相似文献   

渤海辽东湾区海底地形分区特征和成因研究   总被引：3，自引：1，他引：2  

栾振东  李泽文  范奉鑫  阎军  庄丽华 《海洋科学》2012,36(1):73-80

为了探明辽东湾区海底地形,通过测深系统对辽东湾区海底地形进行了高进度、全覆盖测量,进而根据地形起伏特点对辽东湾区海底地形进行了分区,并分析了影响辽东湾地形发育的主要因素。结果表明:辽东湾区海底地形分为5个子区,地形发育受地质构造、水动力来源和沉积物供应的复合影响。  相似文献   

Environmental anomalies in the northeastern East China Sea during the last 3 000 years:implications for El Nio activity in the Holocene     

常凤鸣  李铁刚  庄丽华  阎军 《中国海洋湖沼学报》2010,(1)

To reconstruct the productivity changes for the last 10 500 a in the northeastern East China Sea (ECS),biogenic compounds (such as carbonate,organic carbon and opal),marine micropaleontological fossils (planktonic foraminifera,benthic foraminifera,radiolarian and silicoflagellate) and the compositional characters of benthic foraminifera fauna analyses were carried out on a sediment core DOC082 obtained from the western slope of Okinawa Trough (29°13.93'N,128°08.53'E;1 128 m water depth).The long-term changes of biogenic and micropaleontological proxies display some similarities through the last 10 500 a,which show three different phases:lower values are recorded during the early and middle Holocene (before about 4 000 a BP),followed by an abrupt and remarkable increase at about 4 000 a BP,the late Holocene (after about 3 000 a BP) is characterized by continuously high values.The multi-proxy data of paleoproductivity and percents of benthic foraminifera genera (Uvigerina and Bulimina) show that during the early and middle Holocene (10 500-4 000 a BP) productivity was relatively low with a sudden and distinct increase at about 4 000 a BP,and the late Holocene (3 400-0 a BP) is marked by significantly higher productivity.Also,the radiolarian-based sea surface temperature (SST) records reveal a distinct decline in SST in the late Holocene after 3 200 a BP,very different from the early and middle Holocene.For the last 3 000 a,the enhanced biological productivity and distinctly lower SST indicate a major change of oceanographic conditions in the northeastern ECS.These marine environmental anomalies are consistent with other paleoclimatic records for the late Holocene in the Chinese continent and its surrounding regions.After analyzing the mechanisms of modern productivity and SST changes in the northeastern ECS,and based on the climatic anomalies in the Chinese continent and variations in the Kuroshio Current during modern El Nio periods,we suggest that the anomalous environmental conditions in the northeastern ECS may imply intensified El Nio activity during the late Holocene.  相似文献   

Environmental anomalies in the northeastern East China Sea during the last 3 000 years: implications for El Niño activity in the Holocene     

常凤鸣  李铁刚  庄丽华  阎军 《中国海洋湖沼学报》2010,28(1):190-200

To reconstruct the productivity changes for the last 10 500 a in the northeastern East China Sea (ECS), biogenic compounds (such as carbonate, organic carbon and opal), marine micropaleontological fossils (planktonic foraminifera, benthic foraminifera, radiolarian and silicoflagellate) and the compositional characters of benthic foraminifera fauna analyses were carried out on a sediment core DOC082 obtained from the western slope of Okinawa Trough (29°13.93′N, 128°08.53′E; 1 128 m water depth). The long-term changes of biogenic and micropaleontological proxies display some similarities through the last 10 500 a, which show three different phases: lower values are recorded during the early and middle Holocene (before about 4 000 a BP), followed by an abrupt and remarkable increase at about 4 000 a BP, the late Holocene (after about 3 000 a BP) is characterized by continuously high values. The multi-proxy data of paleoproductivity and percents of benthic foraminifera genera (Uvigerina and Bulimina) show that during the early and middle Holocene (10 500–4 000 a BP) productivity was relatively low with a sudden and distinct increase at about 4 000 a BP, and the late Holocene (3 400–0 a BP) is marked by significantly higher productivity. Also, the radiolarian-based sea surface temperature (SST) records reveal a distinct decline in SST in the late Holocene after 3 200 a BP, very different from the early and middle Holocene. For the last 3 000 a, the enhanced biological productivity and distinctly lower SST indicate a major change of oceanographic conditions in the northeastern ECS. These marine environmental anomalies are consistent with other paleoclimatic records for the late Holocene in the Chinese continent and its surrounding regions. After analyzing the mechanisms of modern productivity and SST changes in the northeastern ECS, and based on the climatic anomalies in the Chinese continent and variations in the Kuroshio Current during modern El Niño periods, we suggest that the anomalous environmental conditions in the northeastern ECS may imply intensified El Niño activity during the late Holocene.  相似文献   

海洋沉积动力过程原位监测平台及其应用     

范奉鑫  阎军  马小川 《海洋地质与第四纪地质》2011,(4):179-185

利用倾斜仪、ADCP、PC-ADP、扇形声纳、OBS等先进仪器组建海洋沉积动力过程原位监测平台,并利用此平台获得了北部湾底部同步连续的波浪数据,流速剖面及近底紊流数据,距底0.5、0.9、1.3m的悬浮物浓度数据以及不同时间的地貌图像.实际观测表明,原位监测平台能够克服极端条件,系统地监测波流、悬浮物浓度以及地貌演化,...  相似文献   

古黑潮演化研究评述   总被引：2，自引：1，他引：1  

向荣  曹奇原  阎军 《海洋科学》2000,24(7):34-37

黑潮是西太平洋海区的重要暖流 ,它携带着高温、高盐水体经台湾东部海域和冲绳海槽北上 ,其主流轴是西北太平洋海气热量交换最强的海区 ,对东亚气候和该区海洋沉积物的分布以及表层生产力的影响巨大。进入晚第四纪以来中国大陆及其邻近海域的古环境变化主要受东亚季风和黑潮暖流的控制［１］,地质历史时期中古黑潮演化的研究 ,对了解东亚古气候变化有重要意义。本文旨在对过去已有的研究成果作简要的评述和分析 ,并对今后的研究提出一些看法和建议。１现代黑潮基本概况黑潮为北太平洋西边界强流 ,与北大西洋西边界的湾流 ,共为世界上最瞩目…  相似文献   

小秦岭西段“太华群”多期构造解析“   总被引：1，自引：0，他引：1  

阎军 《西北地质科学》1992,13(2):75-82

以宏观和显微构造特征为依据,论述了太华群自形成以来的构造演化过程,初步建立了太华群的构造演化序列,揭示了太华群内部的面理置换、褶皱叠加、断裂复合等规律,探讨了各变形幕的构造式样以及构造变形环境。在其构造层次的综合分析基础上,将太华群的构造演化历史,划分为4个主要构造变形阶段:Ⅰ.粘-塑性构造变形阶段;Ⅱ.塑性构造变形阶段;Ⅲ.脆-韧性构造变形阶段;Ⅳ.脆性构造变形阶段。  相似文献   

冲绳海槽北段表层沉积物中底栖有孔虫分布的研究   总被引：1，自引：2，他引：1  

李铁钢  苍树溪  阎军 《海洋与湖沼》1997,28(1):49-55

对1992年5月取自冲绳海槽北段（水深113-1156m，东经126°58.71'-129°9.06’，北纬28°41.75'-31°40.56'）92个表层沉积物中的底栖有孔虫数据进行R型因子分析。分析表明，黑潮流系有4个不同垂直水团的底栖有孔虫群落组合。其中Pseudorotaliaindopacifica,Bolovinarobusta,Cibicidesmargaritiferus,Textulariasaggitula,Cibicideslobatulus和Quinqueloculinaspp.代表黑潮流系的表层水;Hyalineabalthica，Caribeanelladepressa,Cibicidespraecinctus，Planulinawuellerstorfi和Melonisaffinis代表黑潮流系的次表层水;Globobuliminapacifica,Globocassidulinasubglobosa和Trifarinaspp.代表黑潮流系的中层水;Oridorsalistener,Martionottiellaokinawaensis,Pulleniaquinqueloba和Uvigerinadirupta代表黑潮流系的深层水。  相似文献