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1)  North continental slope
陆坡北部
2)  northern slope of the South China Sea
南海北部陆坡
1.
Phylogenetic analysis of bacterial community in deep-sea sediment from northern slope of the South China Sea;
南海北部陆坡深水区沉积物细菌多样性调查
2.
Great efforts have been devoted to the applications of these techniques in gas hydrate exploration on the northern slope of the South China Sea.
本文介绍了海底摄像、电视抓斗、深拖系统和ROV四种海底可视技术,并对海底可视技术在南海北部陆坡天然气水合物勘查中的应用进行阐述。
3.
A high resoluton depositional sequence of late Quaternary has been obtained in core 17940 got from northern slope of the South China Sea.
通过 92个样品分析 ,发现南海北部陆坡末次冰期以来沉积物中有机壁浮游藻类输入通量在新仙女木期和早全新世明显高于其它时期 ,新仙女木期的输入通量峰值及不同于 Spiniferites spp。
3)  northern continental slope of the South China Sea
南海北部陆坡区
1.
Characteristics of Neogene depositional systems on the northern continental slope of the South China Sea and their relationships with gas hydrate;
南海北部陆坡区新近系沉积体系特征与天然气水合物分布的关系
4)  the northern slope of the South China Sea
南海北部陆坡
1.
The calculated result shows that a sediment rate of only 12 cm/ka could be reached if all the materials from Pearl River and Hanjiang River deposited on the northern slope of the South China Sea.
南海北部陆坡是南海海域沉积活动最为活跃的地区之一,发育着迄今为止所发现的南海最高沉积速率堆积体。
2.
This paper presents research showing the occurrence of gas hydrates in the Northern Slope of the South China Sea using the static mode after analyzing 127 thermal data packages.
通过南海北部陆坡获取的127个地热数据,采用静态模式研究其赋存状况。
5)  Continental shelf and slope of the northern South China Sea
南海北部陆架陆坡区
6)  deep-water continental slope area in the northern South China Sea
南海北部陆坡深水区
补充资料:大陆坡
大陆坡
continental slope

   大陆架向海一侧,从陆架外缘较陡地下降到深海底的斜坡。它展布于所有大陆周缘,为全球性地形单元 。大陆坡上界水深多在100~200米之间;下界往往是渐变1500~3500米水深,但在邻近海沟地带,陆坡下延至更深处。大陆坡宽度约为20~100千米以上,总面积计 2870万平方千米,占全球面积5.6%。大陆坡坡度多为3°~6°,1800 米深度以上的平均坡度为 4°17′。大陆坡底质以泥为主,还有少量砂砾和生物碎屑。大陆坡基底为变薄的大陆型地壳。陆坡上还有褶皱、断裂构造,一些陆上构造线可延伸至陆坡。由于河流径流和海洋上升流作用,陆坡沉积物中可含有丰富的有机质,陆坡上有巨厚沉积层的地方具有良好的油气远景。还可有锰结核、磷灰石、海绿石等矿产。在陆坡一些上升流区可形成渔场。
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