1) East China Sea Shelf
东海陆架区
1.
Transport and Burial of Particulate Terrigenous Organic Matter in Changjiang (Yangtze River) and East China Sea Shelf;
颗粒态陆源有机物在长江和东海陆架区的迁移和埋藏
2) East China Sea Shelf
东海陆架
1.
Mesozoic remnant basin characteristics and hydrocarbon exploration direction on East China Sea shelf;
东海陆架中生代残余盆地特征及勘探方向探讨
2.
Space-time contrast of two stages sand ridges on the East China Sea shelf
东海陆架两期沙脊的时空对比
3.
The Mesozoic in the East China Sea Shelf and Taixinan Basin has become a new area of petroleum exploration.
东海陆架和台西南盆地中生界业已成为油气勘探的新领域。
3) East China Sea Continental Shelf
东海陆架
1.
Late Quaternary sedimentary diatom from East China Sea continental shelf and its paleoceanographical significance;
东海陆架晚第四纪沉积硅藻及其古海洋学意义
2.
Correlative study of cone penetration test parameters and physico-mechanical properties of the seabed soil on the East China Sea Continental Shelf
东海陆架海底浅表层土静力触探参数与物理力学指标相关分析
3.
Based on the analysis of core samples from the hole of Zk23 in the East China Sea Continental Shelf and by means of sedimentary stratigraphy, biostratigraphy and chronostratigraphy, thes consider that the fine-sand deposition in borehole was part of buried ancient estuary sand ridges of the Yangtze River.
根据东海陆架Zk23孔岩心分析资料,进行了沉积地层学、生物地层学和年代地层学分析,确定了该钻孔中段细砂层为埋藏古长江河口沙脊沉积,阐明了该孔附近海区冰消期前后和冰后期的沉积历史。
4) continental shelf of the East China Sea
东海陆架
1.
The seasonal changes of the water masses and the dease water circulation on the continental shelf of the East China Sea;
1989年东海陆架水团及高密水环流的季节变化
2.
smectite,illite,kaolinite and chlorite) in <2 μm fraction sediments of the 7 surface samples from the Yangtze Estuary and 258 surface sediment samples from the continental shelf of the East China Sea were analyzed.
对长江口及东海陆架区表层沉积物样品中<2μm粒级组分进行了X射线衍射分析,分别采用上述两种方法计算了样品中4种主要黏土矿物(蒙皂石、伊利石、高岭石和绿泥石)的相对含量,并比较了两种计算结果的差别。
5) the East China Sea Shelf
东海陆架
1.
Quantitative Evaluation of Sediment Provenance on the North Area of the East China Sea Shelf;
东海陆架北部长江、黄河沉积物影响范围的定量估算
2.
Two late Quaternary sediment cores from the East China Sea shelf,EA1 and EA5,have been analyzed for major and trace elements(Si, Al, K, Na, Ca, Mg, Fe, Mn, Ti, P, Li, Ba, Th, Zr, Hf, Cu, Zn, Pb).
东海陆架EA1孔和EA5孔沉积物化学成分变化范围较大,与东海陆架表层沉积物相比,钻孔沉积物的Si、Al、Mg、Mn、Ti、P、Ba、Zr、Co、Ni、Cu、Zn、Cr明显偏高,而Fe、Na、Ca、Sr、Li、U明显偏低,与全球大陆地壳化学组成相比,钻孔沉积物的Si、Li、Rb、Ba、Th、Zr、Hf、Cu、Zn、Pb偏高,而Al、Na、Ca、Mg、Fe、Mn、Ti、P、Sr、U、Co、Ni、V、Cr偏低。
6) East China Sea
东海陆架
1.
Based on seismic records using SIG sparker from a joint Sino French study on marine geology of the East China Sea in 1996,the distribution area of submarine paleodeltas of the Yangtze River(and/or the Yellow River)during the early and middle time of the late Pleistocene is determined.
中更新世晚期东海陆架为一自西南向东北倾斜的广阔的河流冲积平原 ,晚更新世以来自西北方向的大型河流的三角洲受此控制主要发育在东北部较低地区。
补充资料:大东海旅游区
大东海旅游区位于距三亚市区3公里的兔子尾和鹿回头两山之间。月牙形的海湾,辽阔的海面晶莹 如镜,只见白沙融融,阳光、碧水、沙滩、绿树构成了一幅美丽的热带风光图画。这里四季如春,水暖沙平,冬季水温18度,是冬泳避寒胜地和度假休闲者进行潜海观光、海水浴、阳光浴 的理想之地,被国家旅游局评为中国"四十佳"旅游景点之一。
区内海滨度假旅游设施集中而配套,有嬉水乐园、旅游潜艇码头、潜水和跳水基地等,可常年进行多种水上活动和沙滩运动,是目前海南颇具规模的热带海滨旅游度假区。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
参考词条