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英語人>網(wǎng)絡(luò)例句>glacial 相關(guān)的網(wǎng)絡(luò)例句
glacial相關(guān)的網(wǎng)絡(luò)例句

查詢詞典 glacial

與 glacial 相關(guān)的網(wǎng)絡(luò)例句 [注:此內(nèi)容來源于網(wǎng)絡(luò),僅供參考]

The only current ice sheets are in Antarctica and Greenland ; during the last glacial period at Last Glacial Maximum the Laurentide ice sheet covered much of Canada and North America, the Weichselian ice sheet covered northern Europe and the Patagonian Ice Sheet covered southern South America.

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The distribution of glacial-erosion traces on the roche moutonnee has fair regularity, that is to say the long-straight striations were often formed on the top of stoss side and the crescentic scars, crescentic wedges, chatter marks and shorted striations on the end of stoss side and striation of many groups on the flanks, which can show the condition of glacial division-flow.

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Five chalcones were synthesized via the aldol condensation reaction of acetophenone or parasubstituted acetophenones with 1-phenyl-3-methyl-5-phenoxyl-pyrazol-4-aldehyde, which reacted with two kinds of hydrazine in glacial acetic acid under refluxing to give a series of bipyrazoline derivatives. In this synthetic course, glacial acetic acid is not only a solvent, but also a catalyzer.

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The invention relates to a fabric nanometer following cleaning agent for obtaining TiO2/ZnO composite hydrosol, and relative production and cleaning method, wherein it uses butyl titanate and zinc acetate as predecessor, uses glacial acetic acid as catalyst and peptizer, uses water as solvent, uses absolute ethyl alcohol as the solvent of butyl titanate, and uses ethanolamine as deposit agent and supplies OH-, to be hydrolysed and polycondensated to form TiO2/ZnO composite hydrosol. And its components and mass percents are: butyl titanate at 1-15%; zinc diethyl at 1-12%; absolute ethyl alcohol at 1-20%; glacial acetic acid at 5-15%; and aminoethyl alcohol at 0.1-5%, and the left is water. The invention has lower cost and simple process.

本發(fā)明涉及一種可以得到TiO 2 /ZnO復(fù)合水溶膠的紡織品納米后整理試劑及其制備工藝及對織物的整理方法,以鈦酸丁酯和乙酸鋅為前驅(qū)物老年人日批的视频,冰乙酸為催化劑和膠溶劑欧美一区二区操逼,水為溶劑,無水乙醇為鈦酸丁酯的溶劑中文自拍日韩视频在线观看网站,乙醇胺為沉淀劑并提供OH -日韩欧美亚洲综合久久图片,經(jīng)過水解、縮聚反應(yīng)形成的TiO 2 /ZnO納米溶膠整理劑网站三级视频,其組分和重量百分比含量如下:鈦酸丁酯占1~15%亚洲一区二区色图;二水乙酸鋅占1~12%;無水乙醇占1%~20%;冰乙酸占5%~15%免费无遮挡无码永久真人视频观看;乙醇胺占0.1%~5%久久精品国产2020超碰;水余量,具有耐洗性黄色a级片免费网站、無毒91精品欧美一区二区合在线、無刺激、成本低廉色一级A片视频在线播放网站大全、制作工藝簡單可靠的優(yōu)點欧美大胆A级视频69,可實現(xiàn)對對織物的抗紫外、抗菌欧美性爱乱、抗靜電功能整理。

The down core changes of Florisphaera profunda percentage content implied that the thermocline was shallower in glacial periods and deeper in interglacial periods, which might be the direct controlling factors of WPWP productivity changes. It is speculated that the glacial-interglacial fluctuation of the depth of thermocline was induced by the super-ENSO variation.

鈣質(zhì)超微化石下透光帶屬種Florisphaeva profunda百分含量指示的溫躍層深度變化表明冰期溫躍層淺国内自拍第38页、間冰期溫躍層加深卡通动漫亚洲专区第一页,這說明類ENSO式變化導(dǎo)致的冰期-間冰期溫躍層深度波動可能是MIS7期以來暖池核心區(qū)古生產(chǎn)力在冰期高而在間冰期顯著降低的直接控制因素。

Geological evidence for ice ages comes in various forms, including rock scouring and scratching, glacial moraines , drumlins , valley cutting, and the deposition of till or tillites and glacial erratics .

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More : glacier, glacial river, glacier stream, ice stream, glacial stream

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This photo shows the end of the Muztag Glacier. Moraines are on the right of the glacier, with a small glacial lake beyond it. Submerged glacial gravels can be seen clearly.

該照片反映的是木孜塔格冰川的末端,冰川右側(cè)為冰磧物久久免费一级黄色视频,前下方為小型的冰川湖一级黄色av,冰川沉礫清晰可見。

A kettle is a steep-sided, usually basin- or bowl-shaped hole or depression without surface drainage in glacial-drift deposits, often containing a lake or swamp, and believed to have formed by the melting of a large, detached block of stagnant ice (left behind by a retreating glacier) that had been wholly or partly buried in the glacial drift.

鍋穴是指邊緣陡峭的盆形或碗狀孔洞或凹陷又长又大又硬黄色,在冰磧沉積物表面沒有水系黄片毛片av,通常包圍著湖泊或沼澤。通常認為是冰川退縮過程中停滯于冰川沉積物中的巨大冰塊融化而形成的亚洲一区精品黄,一般10-15米深一级做a爰片久久毛片A片美国,直徑達30-150米。在加拿大平原地區(qū)有很多第四紀冰川退縮所形成的鍋穴湖泊就用 kettle lake 表示欧美福利午夜。

This thesis has systematically dealt with the glacial, lake and climatic fluctuations in the areas mentioned above throughout the late stadial of the Last Glaciation, based on synthetical records of glacial development at the high mountains, lacustrine stratigraphy and lake evolution in both the high plateau basins and the lower altitude interior ones, periglacial phenomena and palaeosols as well as microfossils in deposits.

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