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marine     
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  海洋
    The Microbioremediation of Polycyclic Aromatic Hydrocarbons (PAHs) Pollution in Marine Environment
    海洋环境中多环芳烃污染的微生物修复作用研究
短句来源
    Study on the Spatial Relational Model for the Division of Marine Functional Zonation and the Implementation under GIS
    海洋功能区划中的空间关系模型及其GIS实现(以莱州湾为例)
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    Studies on Organic Pollutants' Oxidative Degradations by Photo-assisted Fenton Method and Their Sorption Behaviors on Marine Sediments
    有机污染物的光助Fenton法氧化降解及其在海洋沉积物上的吸附行为研究
短句来源
    Simulated Experimental Study on Several Significant Problems Related to Marine Gas Hydrate
    海洋天然气水合物若干问题的模拟实验研究
短句来源
    Fast Filtering Decomposing Signal into Intrinsic Mode Function and Its Applications in Marine Data Analysis
    快速滤波本征模态信号分解及其在海洋数据分析中的应用
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  海相
    The revelation of marine lower Cretaceous series in east area of China and its geological significance
    我国东部海相下白垩统的发现及其地质意义
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    DIVISION AND ENVIRONMENTAL EVOLUTION OF LATE QUATERNARY MARINE BEDS OF S 3 HOLE IN THE BOHAI SEA
    渤海南部S_3孔晚第四纪海相地层的划分及环境演变
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    Study on the disintegration of marine stratum in the northern shelf region of nearshore seas of China
    中国近海北部陆架海相地层解体问题的研究
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    Mesozoic marine sediment identification and distribution in the eastern Pearl River Mouth basin
    珠江口盆地东部海相中生界识别及分布
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    Identification of effective hydrocarbon source rocks in marine strata in the Jianghan basin,Chian
    江汉盆地海相地层有效烃源岩的识别
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  海上
    A Boundary Layer Model for the Estimation of Marine Surface Winds
    海上风的边界层模式
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    THE APPLICATION OF NAVIGATION GPS DATA IN MARINE GEOPHYSICAL EXPLORATION ──PROCESSING OF RANDOM NOISE IN GPS NAVIGATION DATA
    导航型GPS在海上地球物理勘探中的应用──卫导数据随机噪声处理
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    Operation Technology of Marine Drilling in Sandouao Bay, Ningde,Fujian Province
    福建宁德三都澳海上钻探施工技术
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    Research on the methods of assessment of training in marine oil spill crisis response simulator
    海上溢油应急反应模拟训练评估方法的研究
短句来源
    The Research and Development of Electronic Chart System of Marine Oil Spill Response
    海上溢油应急反应电子海图系统的研制开发
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  海水
    A Preliminary Study on the Use of Tradescantia Micronucleus Technique in Monitoring Marine Pollution
    用紫露草微核技术监测海水污染的初步研究
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    MARINE GEOCHEMISTRY OF NITROGEN NEAR ESTUARY OF YANGTZE RIVER Ⅲ ORGANIC NITROGEN IN SEA WATER NEAR ESTUARY
    长江口附近氮的地球化学 Ⅲ.海水中的有机氮
短句来源
    137 Cs contents in the marine organisms, seawater and sediment in Dayawan before and after the nuclear power plant operation
    核电站运行前后大亚湾海洋生物、海水和沉积物~(137)Cs含量
短句来源
    A method of determination of total phosphate in theseawater and marine sediment
    海水和海洋沉积物中总磷的测定
短句来源
    PRIMARY δ~(13)C ANDδ~(18)O VALUES IN MARINE CARBONATES AND THE SEA WATER TEMPERATURE OF DENGYINGXIA AGE IN SOUTH CHINA
    中国南方灯影峡期海洋碳酸盐岩原始δ~(13)C和δ~(18)O组成及海水温度
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  marine
ROLE OF INTERMEDIARY BIOMARKERS IN DETERMINING THE ANTICANCER EFFICACY OF MARINE COMPOUNDS
      
In the present study, two of the probable an umor marine compounds, manzamine A and sarcophine, were screened using benzo[a]pyrene (BP)-derived DNA adduct formation in MCF-7 cells as intermediary biomarker.
      
The results show that low concentrations of NO were self-produced by marine algae during the exponential growth period and were about nmol/L level.
      
The NO threshold concentration exists according to the influence of exogenous NO on the marine phytoplankton growth.
      
Characterization of iodine species in the marine aerosol: To understand their roles in particle formation processes
      
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For the purpose of application of some geochemical indicators in determining of sedimentary environment of the Funing Group, Jin-Hu Depression, Jiangsu Province, more than 600 coring mud samples of this Group, through analyzing the trace elements by using emission spectograph, have been investigated. For testing the validity of such interpretation, 22 modern known marine and freshwater mud samples have also been analyzed. The results indicate that, the paleosalinities of the Second and Fourth members of...

For the purpose of application of some geochemical indicators in determining of sedimentary environment of the Funing Group, Jin-Hu Depression, Jiangsu Province, more than 600 coring mud samples of this Group, through analyzing the trace elements by using emission spectograph, have been investigated. For testing the validity of such interpretation, 22 modern known marine and freshwater mud samples have also been analyzed. The results indicate that, the paleosalinities of the Second and Fourth members of the Funing Group are both higher than that of the normal freshwater mud. It has been suggested that transgressions had occured during those periods of deposition. Such conclusion is in agreement with the results what the palaeontological and mineralogical studies have been achieved.

本文主要通过苏北金湖凹陷下第三系阜宁群的岩心及部分现代海湖底质样品,进行了岩石化学、光谱分析;利用硼、镓、铷、锶、钡、钾等几种微量元素含量及其比值,以及沉积磷酸盐的分析,和其组分比,进行沉积环境的分析。其分析结果与该地区的岩石矿物分析,古生物分析等相吻合,表明该区曾有过海水侵入的影响。

Data from the qualitative and quantitative micropaleontological analyses of more than 20 cores provided abundant informations concerning Quaternary marine transgressions in Shanghai and its environs. The Quarternary Period in Shanghai region witnessed four marine transgressions with different intensity. The transgressions of Middle Pleistocene and the early Late Pleistocene were weak and represented by deposits of the transitional nature from marine to continental facies only. The strongest...

Data from the qualitative and quantitative micropaleontological analyses of more than 20 cores provided abundant informations concerning Quaternary marine transgressions in Shanghai and its environs. The Quarternary Period in Shanghai region witnessed four marine transgressions with different intensity. The transgressions of Middle Pleistocene and the early Late Pleistocene were weak and represented by deposits of the transitional nature from marine to continental facies only. The strongest transgression occurred in middle Late Pleistocene when shallow-marine deposits were accumulated. The strata of the Holocene transgression which is relatively strong may be subdivided stratigraphically into three parts. As shown by the horizontal distribution of Foraminifera, the intensity of Quaternary transgression is stronger in the east of Shanghai region than in the west. The comparison between micropaleontological and palynological data in Shanghai region has revealed a close correlation between sea-level changes and climatic fluctuations. In the light of the paleoecology of Foraminifera, Ostracoda and other groups of microfossils, as well as the sedimentological, palynological and archaeological data, this paper discusses in detail the depositional environments, the limits of transgressions and their geological ages during Quaternary time in Shanghai region.

根据微体古生物分析结果并综合其他资料,证明上海地区东部第四纪以来经历过四次海进:晚更新世中期和全新世的海进较强,形成浅海相沉积;中更新世与晚更新世早期的海进较弱,仅有海陆过渡相沉积。

The paper divides the Ouaternary Sedimentary strata in shanghai region into twelve sedimentation units by analysis of the lithological charactors and lithofacies got from the study of about 200 deep cores and 300 shallow cores in the region of shanghai.In addition based on analy- sis of sporo-pollen and microfossls,this paper gives the correspondent zones of the sporo-pollen composition and distribution of the land and marine deposits The accordance with the features of the sedimentary structure and the...

The paper divides the Ouaternary Sedimentary strata in shanghai region into twelve sedimentation units by analysis of the lithological charactors and lithofacies got from the study of about 200 deep cores and 300 shallow cores in the region of shanghai.In addition based on analy- sis of sporo-pollen and microfossls,this paper gives the correspondent zones of the sporo-pollen composition and distribution of the land and marine deposits The accordance with the features of the sedimentary structure and the nature of sporo-pollem compositions the Quaternary period might be derided into five cold stages,with foul intevening warm stages and the post-glacial stage.In order of time we denominated them as:Chung-min cold stage,Hu-Xi cold stage;Hu-Dung cold stage,Zha-Bei cold stage and Su-Zhou River cold stage.In terms of the date of microfossils and lith- oracies,they represent five marine transgressions with different scopes of activity corresponding to the above warm stage and the post-glacial stage.We denominated them as Jiang-Zheng transgression,Deng-Zhen transgression,Xi-giao transgression,Chao-Jia-Du transgression and Wai- Tau transgression. In the cold stage,lacustrime facies dominaten the deposits.In the warm stage,followed by the transgression,most of the deposits represent themselves as fluviatile facies with marine deposits in same parts of the region According to the method used in Palaeorlimatdogy and stratigraphic division,the Quaternary strata in Shanghai region may be divided as: ancient Pleistocene (stratal2—11);Early Pleistocene (strata10—9) middle Pleistocene (strata8—7);Late Pleistocene (strata6—3);new Pleistocene (strata2),and Holocene (strta1).

本文通过对上海地区约200个深孔和300个浅孔的岩性、岩相分析,把本区第四纪沉积层归纳为十二个沉积单元,并根据孢粉与微古分析资料得出与之相应的孢粉组合带及海陆相沉积。从沉积结构特征和孢粉组合特点,得出第四纪时期本区有五个寒冷期及与之相间的四个温暖期和冰后期,自早至晚分别命名为:崇明寒冷期、沪西寒冷期、沪东寒冷期、闸北寒冷期、苏州河寒冷期、根据微古和岩相等资料,发现有同温暖期和冰后期相呼应的五次不同范围的海浸,自早至晚命名为:江镇海浸、邓镇海浸、西郊海浸、曹家渡海浸和外滩海浸。在寒冷期以湖相沉积为主,在温暖期以河流相沉积为主,局部地区为海相沉积。按古气候地层划分原则,把本区第四纪地层划分为:古更新统(层12-11);早更新统(层10-0);中更新统(层8-7);晚更新统(层6-3);新更新统(层2),和全新统(层1)。

 
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