Through the analysis of the stratigraphy and sedimentary facies of the research areas , the description model between the stratigraphic framework and deposite environment can be set up firstly by the transition from the " three horizons sandstone with two intercalated limestone horizons ' mn yanshiping area to shale and marl in amdo - zigetang co , and to oil shale in bilong co , then by the transition of the shallow water platform facies to the deep water continental shelf , slope , and to the deep water basin 通过对研究区地层和沉积相分析，建立起一个从北向南由雁石坪地层类型“三砂夹两灰”过渡为安多?兹格塘错地层类型泥页岩、泥灰岩，最后到比洛错地层类型黑色油页岩，由浅水台地相过渡到深水陆棚、斜坡，最后到深水盆地相的地层格架与沉积环境解释模式。
What makes this island special is that it is the only oceanic island not connected to the continental shelf in malaysia rising 2 , 000 feet 600 meters on a limestone pinnacle that mushrooms out near the surface . pulau sipadan have the largest variety of soft corals in the world . turtles swim and frolic freely in the waters around sipadan and divers will find lobster , barracudas , beautiful coral fishes and sometimes even sharks swimming by 其蘑菇形石柱岛，深入海底1000米，露出地面的浅水处，各式咸水鱼成群，不谙泳术只玩浮潜，也够大开眼界深谙潜水者，当然是到深海峭壁探险，在水深30米跟成群大海铁头鱼鲨鱼及东星斑等来个大合照。
On the basis of former researchers ' work , the author studies sm on ecs continental shelf according to mathematical simulation technique . firstly , the author simulates marine dynamic field with much precise temperature and salinity data . seconly , the author computes the distribution of concentration of sm and its transport in winter and in summer according to a 3 - d suspended matter model . lastly , the author analyses the transport of suspended matter by sea water dynamic circumstance 本文在前人的工作基础上，通过数值模拟的方法就悬浮体输送问题进行了探讨。首先，利用精度较高的温盐资料模拟了黄、东海的水动力场，再通过一个对流? ?扩散型物质输送模型模拟了东海陆架上冬季和夏季悬浮体的分布情况，最后结合水动力就悬浮体输送进行了分析。
The shallow thermocline distributes in the areas of guangdong , guangxi , fujian and vietnam continental shelf , with obviously seasonal variabilily , and at the same time , in the south and middle areas of nanhai , even in winter when there is no thermocline in the coastal area , there also exists the shallow thermocline 后者广东、广西、福建沿海陆架区则与黄、东海相同，表现为季节性温跃层，有成长、强盛、消衰、无跃层的年周期变化过程。南海深温度跃层基本属于水团叠置型，跃层分布范围及跃层强度、上界深度、厚度与气候关系不大。
According to the differences of sedimentary facies and environment , the source rock are divided into four types such as lime - mud reef in platform margin , platform inner sag , deep - water flat slope or continental shelf , abyssal basin , the lime - mud reef type is distributed in platform margin of upper ordovician , the remained three types are widely distributed in cambrian - ordovician system 根据沉积相带与沉积环境的不同，可将烃源岩划分为在不同沉积环境中的4种类型烃源岩；台地边缘灰泥丘型烃源岩、台地内凹陷型烃源岩、深水缓坡与陆棚型烃源岩、深海盆地型烃源岩。
The topography and the physiognomy of the south china sea are very complex such as continental slop , continental shelves , seamounts , sea basin , etc . the south china sea lies between qingzang plateau , which is as the main driver of the variety of climate , and the western part of the pacific , which is called warm pool , and is influenced by some current systems , such as coastal current , kuroshi , etc . the south sea has considerable species 南海具有陆坡、陆架、海沟、海盆等复杂的地形、地貌；南海位于作为地球气候变化的主要驱动力的青藏高原和西太平洋暖池之间；南海受到沿岸流、南海暖流水、黑潮入侵水等流系的影响；南海具有丰富的物种分布；上述因素共同影响南海生源要素的分布、输送和迁移。
The transitional facies can also be divided as estuarine , tidal flat and lagoon ; the depositional envirnononents of clastic rock marine facies include offshore , shallow water continental shelf , deep water continental shelf , slop as well as the deep water basin ; the carbonate facies can also be divided into a carbonate platform and ramp 海陆过渡相又分为河口湾、潮坪、泻湖；海相碎屑岩沉积环境包括滨海、浅水陆棚、深水陆棚、斜坡以及深水盆地；碳酸盐岩海相又可分为碳酸盐台地、碳酸盐缓坡。
The juridical continental shelf of a coastal or island nation consists of the seabed and subsoil of the submarine areas that extend beyond its territorial sea to the outer edge of the continental margin , or to a distance of 200 nautical miles from the baseline used to measure the territorial sea where the continental margin does not extend to that distance 书上的翻译：沿海国或者岛国法律上的大陆架包括延伸到其领海以外直到大陆边缘外部界限的海底区域的海床和底土;如果从测算领海宽度的基线起到大陆边缘的距离不到200海里，则应扩展到200海里的距离。
