On April 27, alexandrine sea hands in Chinese sea oil to sign strategic framework agreement greatly, build cooperation Chinese sea oil, Shanghai to hand in research center of technology of project of big deep water and Chinese sea oil, Shanghai to make research center of technology of project of great new energy resources.

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The evolution of tides and tidal currents on the continental shelves of the Bohai Sea, Yellow Sea and East China Sea has deeply influenced the sediment transport and deposition as well as the formation, distribution and evolution of sea bottom topography since the Last Deglaciation.

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The first one is to build a slope of certain gradient and length according to the main direction of sea-ice movements at coast, to make the sea-ice assembling under the slope climb along the slope by virtue of environmental driving force of wind and flow, and then to take out sea-ice cubes to desalinize after sea-ice falling into the ice-storing section when it reaches the top of the slope.

一是在岸邊按海冰運(yùn)動(dòng)的主方向修建有一定坡度和長度的斜坡，利用環(huán)境驅(qū)動(dòng)力的作用操操操射射射干干干，使聚集在斜坡下的海冰沿著斜坡向上爬升禁止18岁以下的看A片，上升到坡頂后跌入貯冰區(qū)內(nèi)，再從貯冰區(qū)中取出海冰塊進(jìn)行淡化韩国产三级三级香港三级日本三级。

The study shows that in various continental downfaulted basins in eastern China,the China East Sea basin of the southeast sea region and the continental shelf—Qiongdongnan basin and Zhujiangkou basin—of the northern South China Sea,CO2 in CO2 reservoirs and CO2-rich oil/gas reservoirs is of typical volcanic mantle-derived type and that its migration and concentration is mainly controlled by mantle-derived volcanism and gas-conducting distribution of deep basement faults connected with the gas source at depth. CO2 is mainly sourced from substantial amount of CO2 associated with mantle-derived volcanism at the deep level of the crust. CO2 in the CO2 reservoirs and CO2-rich oil/gas reservoirs in the Yinggehai basin on the continental shelf of the northern South China Sea is of crust origin and crust-mantle mixing origin and mainly controlled by local,layer-by-layer and zone-by-zone,multiple intrusion of late hydrothermal fluids in mud diapir areas and physico-chemical processes of very thick Pliocene-Miocene marine calcareous sandstone and mudstone.

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Dependent on the past research in seaice, in Bohai Sea, in 2003-2004 winter and 2004-2005 winter with level ice for the target we open the field experiments to study the essential spectrum characteristic of ice, removing by testing means various nonessential factor for sea water in the fixing big ice plate, building up 170 growth conditions to look like under the natural condition, the growth expect different sample series; in 2004-2005 winter and 2005-2006 winter continue two pass to break thorough Bohai Sea in the ship to collect 59 sea ice sample that have the non-essential ice factors in winter, open the influence research that the field hangs sand to contribute to the spectrum of the ice body; in 2005-2006 winter, fast ice to open the field spectrum curves to coast and analytical research.

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At that time, now the Bohai Sea, Yellow Sea and East China Sea, the Sea of Japan area, are on land, is part of Laurasia.

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