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971.
972.
矿产资源贫乏,平原面积狭窄是日本谋求发展的重大障碍。向海洋扩展土地,追求土地的最佳利用方式,推动着日本填海造陆的历史,创造出日本列岛独具特色的海岸线景观。本文主要阐述日本人造陆地的发展历史,并具体介绍其人造陆地利用形态的发展变化特征。 相似文献
973.
Altimeter and in situ data are used to estimate the mean surface zonal geostrophic current in the section along 115°E in the southern Indian Ocean,and the variation of strong currents in relation to the major fronts is studied.The results show that,in average,the flow in the core of Antarctic Circumpolar Current(ACC) along the section is composed of two parts,one corresponds to the jet of Subantarctic Front(SAF) and the other is the flow in the Polar Front Zone(PFZ),with a westward flow between them.The mean surface zonal geostrophic current corresponding to the SAF is up to 49 cm · s-1 at 46°S,which is the maximal velocity in the section.The eastward flow in the PFZ has a width of about 4.3 degrees in latitudes.The mean surface zonal geostrophic current corresponding to the Southern Antarctic Circumpolar Current Front(SACCF) is located at 59.7 °S with velocity less than 20 cm · s-1.The location of zonal geostrophic jet corresponding to the SAF is quite stable during the study period.In contrast,the eastward jets in the PFZ exhibit various patterns,i.e.,the primary Polar Front(PF1) shows its strong meridional shift and the secondary Polar Front(PF2) does not always coincide with jet.The surface zonal geostrophic current corresponding to SAF has the significant periods of annual,semi-annual and four-month.The geostrophic current of the PFZ also shows significant periods of semi-annual and four-month,but is out of phase with the periods of the SAF,which results in no notable semi-annual and fourmonth periods in the surface zonal geostrophic current in the core of the ACC.In terms of annual cycle,the mean surface zonal geostrophic current in the core of the ACC shows its maximal velocity in June. 相似文献
974.
Deformation bands formed during soft-sediment deformation: Observations from SE Utah 总被引:1,自引:0,他引:1
Several types of syndepositional deformation structures contain strain localization structures known as disaggregation bands. Abundant field examples from Utah show that such bands can be related to vertical movements linked to loading and fluid expulsion, forming a pre-tectonic set of strain localization structures in deformed sandstones that can easily be overlooked or misinterpreted as tectonic structures in petroleum reservoirs. Plug measurements and thin-section investigations show that they have little or no influence on fluid flow. In contrast, disaggregation bands formed as a response to tectonic stress at higher confining pressures (depths) in the same lithology show up to 3–4 orders of magnitude reduction in permeability. This makes it important to distinguish between synsedimentary and tectonic deformation bands. They should also be separated because only bands formed in relation to tectonic stress can be used to predict nearness to important faults and to assess the extent of faulting in a reservoir. 相似文献
975.
Valérie Ballu Jérome Ammann Olivier Pot Olivier de Viron Glenn S. Sasagawa Gilles Reverdin Marie-Noelle Bouin Mathilde Cannat Christine Deplus Sébastien Deroussi Marcia Maia Michel Diament 《Journal of Geodesy》2009,83(2):147-159
Decades of cruise-based exploration have provided excellent snapshots of the structure of mid-ocean ridges and have revealed
that accretion is a mixture of steady-state and quantum events. Observatory-type studies are now needed to quantify the temporal
evolution of these systems. A multi-disciplinary seafloor observatory site is currently being set up at the Lucky Strike volcano,
in the axial valley of the slow spreading Mid-Atlantic ridge as a part of the MoMAR (monitoring of the Mid-Atlantic Ridge)
initiative. The aim of this observatory is to better understand the dynamics of the volcano and the hydrothermal vents hosted
at its summit as well as their plumbing systems. In August 2006, the GRAVILUCK cruise initiated an experiment to monitor the
deformation of Lucky Strike volcano. A geodetic network was installed, and seafloor pressure, gravity and magnetic data were
collected. In this paper, we present the method used to monitor volcanic deformation, which involves measuring relative depth
difference between points within a seafloor geodesy network. We show that, taking into account oceanographic variability and
measurement noise, the network should be able to detect vertical deformations of the order of 1 cm. 相似文献
976.
根据实际公路边坡工程的特点,选取具有代表性的断面和该边坡位移监测的跟踪监测点,用位移监测桩监测边坡的表层位移和多点位计监测边坡的深部位移,反映出边坡在开挖过程中的实际状态。监测数据与研究结果表明,位移监测对边坡施工过程中的稳定性评价具有指导作用,得出了边坡实际变形方式,监测结果与实际调查相吻合。 相似文献
977.
978.
冬季南海北部陆架锋区悬浮颗粒态硅的分析 总被引:2,自引:1,他引:1
对冬季南海北部陆架锋区的悬浮颗粒态生物硅(Particulate Biogenic Silica,PBSi)和成岩硅(Lithogenic Silica,LSi)含量进行了调查分析,讨论了悬浮颗粒态生物硅分布及其影响因素。结果表明,南海北部陆架区悬浮颗粒态生物硅和成岩硅平均含量分别为0.59和8.93μmol/dm3。生物硅分布与水团关系密切:在营养盐充足的沿岸水生物硅含量高(1.0μmol/dm3);而在营养盐缺乏的陆架表层水生物硅含量低(0.23μmol/dm3);在两种水团过渡区生物硅含量居中(0.65μmol/dm3)并与溶解硅酸盐(Dissolved Silicate,DSi)成显著正相关(R=0.48,N=44,P=0.001,a=0.01)。此外锋面位置也直接影响生物硅的含量与分布。大部分调查海区被高温高盐低营养盐海水占据,因此导致了调查海区以低浓度的生物硅和成岩硅为特征,且与世界其他海区相比,生物硅含量处于低值区。 相似文献
979.
黄海暖流源区海表面温度锋面的结构及季节内演变 总被引:2,自引:0,他引:2
利用1985~2002年月均和每8天平均的AVHRR Pathfinder卫星海表面温度数据,分析了黄海暖流源区海表面温度锋面的分布特征及其季节和季节内演变过程的规律.分析结果表明,黄海暖流源区海表面温度锋面只在冬季及其前后出现,且是一个包含南北两支锋面的锋面系统,其北支锋面位于33°~34°N之间,大体呈东西走向,南支锋面沿长江浅滩边缘,呈西北东南走向,作者称之为黄海暖流源区锋面.该锋面从11月下旬于济州岛西部生成并向西北方向扩展,至1,2月份达到最大程度,于2月下旬后向东南方向退缩并在3月份至5月份之间消失.在该锋面系统的生长期和衰退期,其南北两支锋面有时于西端连接在一起而形成指向西北的舌状锋面.黄海暖流源区锋面的演变过程与黄海暖流的演变过程紧密相关,也对黄东海的质量和热量交换有重要影响. 相似文献
980.