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中国新疆
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  xinjiang china
     The major proteinaceous components of two strains of Borrelia burgdorferi XjI3 and XjI12 iso- lated from Xinjiang,China and their biological characteristics were analysed by SDS-PAGE and Western blot.
     作者用Discontinuous SDS一PAGE及Western blot分析了两株分离自中国新疆的Borrelia burgdorferi─—XjI_3和XjI_(12)株的主要蛋白组分及其生物学属性。
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     The Management and Sustainable Utilization of the Grassland in Xinjiang, China
     中国新疆草地的管理与可持续利用
     Three new species in Polygonum section Polygonum (Polygonaceae) from Xinjiang, China, are described and illustrated.
     描述了中国新疆蓼科Polygonaceae蓼属萹蓄组PolygonumsectionPolygonum3新种。
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     APPLICATION OF REMOTE SENSING GEOLOGY TO NORTHERN XINJIANG, CHINA
     中国新疆北部遥感地质找矿的应用
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     The Chronological Characteristics of Bosten Lake Holocene Sediment Environment in Xinjiang, China
     中国新疆博斯腾湖全新世沉积环境年代学特征
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  xinjiang of china
     Britain and Xinjiang of China in Modern Times, 1840-1911
     近代英国和中国新疆(1840-1911)
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     The Vegetation Classification Using FVC and DEM in South Xinjiang of China
     利用FVC和DEM对中国新疆南部植被的分类研究
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     Chapter one outlines the early relationship of Britain and Xinjiang of China.
     第一章论述了早期英国和中国新疆的关系。
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     A Review on the Studies of the Relationship between UK and Xinjiang of China in Modern Times
     近代英国和中国新疆关系研究述评
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     Study on Cooperation in Economy and Trade of Xinjiang of China and Kazakhstan
     中国新疆与哈萨克斯坦经贸合作研究
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  “中国新疆”译为未确定词的双语例句
     The significance of the data was analyzed by χ2 testThe frequencies of the CCR5-Δ32、CCR2b-64I and SDF1-3'A were as follows:2.14%、18.81% and 22.86%,respectively.
     CCR5-Δ32、CCR2b-64I和SDF1-3'A在中国新疆地区IDUs中的突变基因频率分别为:2.14%,:18.81%和22.86%。
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     96.5%~98.9% with the Xinjiang epidemic strain of HEV CH 1.1;
     与HEV中国新疆流行株CH1.1同源性为96.5%~98.9%;
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     Genetic polymorphism of 3 STR loci of CSF1PO,TPOX and TH01 in Chinese Kazak ethnic population
     中国新疆哈萨克族人群CSF1PO、TH01和TPOX三个STR位点的遗传多态性
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     Teleseismic Body Wave Broadband Analysis on Source Process of the Southern Xinjiang Earthquake with Mb6. 2 of 2 October, 1993 in China
     用远震体波宽频带记录分析1993年10月2日中国新疆南部Mb6.2地震的震源过程
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     Study on the FUT2 gene structure of Xinjiang Uighur people of China
     中国新疆维吾尔族人群FUT2基因结构的研究
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  xinjiang china
The photoluminescence and excitation spectra of sodalites from Greenland, Canada and Xinjiang (China) are observed at 300 and 10?K in detail.
      
Zonation of flora and vegetation of the Northern declivity of the Karakoram/Kunlun mountains (SW Xinjiang China)
      
Isolation and Identification of Hepatitis E Virus in Xinjiang China.
      
  xinjiang of china
The glass samples were unearthed from Hunan, Hubei, Yunnan, Sichuan, Guizhou, Guangdong and Xinjiang of China.
      
Holocene abrupt climate shifts and mid-Holocene drought intervals recorded in Barkol Lake of Northern Xinjiang of China
      
Water Resources, Land Exploration and Population Dynamics in Arid Areas - The Case of the Tarim River Basin in Xinjiang of China
      


It is difficult to determine the initial Sr isotopic composition exactly by the whole rock Rb-Sr isochron method, especially for altered and weathered basic rocks and pegmatites, baeause basic rocks are Rb-poor and Sr-rich, and pegmatites, especially granite-pegmatite, are highly rich in Rb and poor in St, and with coarse and large mineral crystals.The authors have systematically studied the mineralogy and Sr isotopic geochemistry for over two hundred apatites in granites of differeut genetic types over extensive...

It is difficult to determine the initial Sr isotopic composition exactly by the whole rock Rb-Sr isochron method, especially for altered and weathered basic rocks and pegmatites, baeause basic rocks are Rb-poor and Sr-rich, and pegmatites, especially granite-pegmatite, are highly rich in Rb and poor in St, and with coarse and large mineral crystals.The authors have systematically studied the mineralogy and Sr isotopic geochemistry for over two hundred apatites in granites of differeut genetic types over extensive regions in China, which saggests that the Sr isotopic composition of the primary apatites formed in the early stage of crystallization may well show the initial ~(87)Sr/(86)Sr ratio (~(87)Sr/~(86)Sr); values at the time of solidification of relevant granites. Apatite, having very stable crystal chemical structure, is very good for the retention of Rb and Sr and is strong to resist weathering. The apatite content is high in some basic rocks and pegmatites, for example, ia apatite-bearing gabbro and arfvedsonite-diopside-apatite pegmatite it is up to 5%. Therefore, it is an economic, qaick and effective method to study the sr iuotopic composition of apatite from the above-mentioned rocks in order to probe into their petro-genesis, material source and geochemical process.

利用磷灰石,测定了中国新疆、内蒙、福建、云南西部的伟晶岩,以及四川、云南、江苏、河北等地基性侵入岩的Srl_((?)p);并根据锶同位素组成特征,结合地质条件提供的限制,划分出:幔源型伟晶岩(SrI_(ap)为0.7026—0.7033);壳源型伟晶岩(SrI_(2p)为0.7110—0.7145),它们各具不同的特征矿化。以及SrI_(ap)〈0.705与SrI_(ap)为0.7080—0.7107两组不同的幔源型墓性岩体。并讨论了磷灰石锶同位素测定方法,在理论和实践运用上的意义.

The gold deposit dealt with in this paper has been proved to be a new type ofgold deposit. It formed within a hot spring system of the ancient oceanic crustwhich was then emplaced onto the continent along with the marine-crustal struc-ture. This deposit consists of the Sartohay and Anqi metallogenic balts, equivalent tothe south subbelt and north subbelt of ophiolite, respectively. In the Sartohay belt,the gold bodies are found in basalts, ultramafic rocks and their altered rocks, andin the Anqi belt, in basalts...

The gold deposit dealt with in this paper has been proved to be a new type ofgold deposit. It formed within a hot spring system of the ancient oceanic crustwhich was then emplaced onto the continent along with the marine-crustal struc-ture. This deposit consists of the Sartohay and Anqi metallogenic balts, equivalent tothe south subbelt and north subbelt of ophiolite, respectively. In the Sartohay belt,the gold bodies are found in basalts, ultramafic rocks and their altered rocks, andin the Anqi belt, in basalts and pyroclastic-sedimentary rocks. The two belts aredifferent in mineral composition. Pyrite in the Sartohay bult is rich in Co and Nibut poor in As, while the reverse is the case with that in the Anqi belt. The min-eral characteristics and inclusion thermometry seggest that both ore-forming tem-perature and pressure in the Sartohay metallogenetic belt are higher than those inthe Anqi Inetallogenic belt. The sulfur isotopic composition in the deposit indicates that the sulfur camefrom the upper mantle. The hydrogen and oxygen isotopic compositions suggest thatthe ore-forming hydrothermal fluid was a metamorphic hydrothermal mixture ofmagmatic water and sea water, equivalent to that of ophiolite. The Pb isotopic ageof the ores was dated at 290-320Ma, implying that the deposit was formed almostsimultaneously witb the ophiolite. The evidence shows that the formation of the Toligold deposit was related to the convection of submarine hydrothermal solution andas well a product of the submarine hot spring activities.

中国新疆西准噶尔托里县境内的安齐-萨尔托海一带的金矿床,产在达拉布特蛇绿岩带的蛇绿岩套中。根据金矿床的地质背景、地球化学特点和成矿温度等,作者将其成因与古洋壳的热泉活动联系起来,认为产于蛇绿岩?不同部位的金矿床和矿化系同一成因,并建议命名为蛇绿岩型金矿,

The Kelamaili Region is located in the southern part of the Kelamaili deep fracture of the eastern Junggar region in Xinjiang, analogous to the western part of the Tuvaella biographical province. Based on lithologics and biotic association character, the Silurian strata in the region can be divided into Middle and Upper Series as follows: the Middle Silurian -Baishanbao Formation, the lower part of the Upper Silurian-Hongliugou Fm., the upper part of the Upper Silurian-kushuiquan Fm.

根据岩性和生物组合特征,该区的志留纪地层划分为:中志留统白山包组,上志留统下部红柳沟组,上部苦水泉组.白山包组为粉砂岩和细砂岩,夹钙质砂岩和少量砾岩,钙质砂岩中含腕足类化石:Tuvaella rackovskii,T.gigangea, Stegerhynchus angaciensis,Tannusp-irifer,Spiriferina,Zygospiraella,Resserella obicularia,Leptostrophia elegestica等,以及三叶虫:Encrinurus.红柳沟组为钙质细砂岩、泥质灰岩、生物碎屑灰岩,灰岩中化石十分丰富,含床板珊瑚:Favosites cf.[zhifangensis,Mesofavosites shang-siensis,Hil aepora,Pseudoplasmopora;四射珊瑚:Amsdenoides,Laccophyllumetc.:三叶虫:Encrinurus,Phacops:头足类:Geisonoceras,Michelinoceras等.与白山包组整合接触.苦水泉组整合在红柳沟组之上,为中厚层状凝灰质粉砂岩、细砂岩、沉凝灰岩,夹少量钙...

根据岩性和生物组合特征,该区的志留纪地层划分为:中志留统白山包组,上志留统下部红柳沟组,上部苦水泉组.白山包组为粉砂岩和细砂岩,夹钙质砂岩和少量砾岩,钙质砂岩中含腕足类化石:Tuvaella rackovskii,T.gigangea, Stegerhynchus angaciensis,Tannusp-irifer,Spiriferina,Zygospiraella,Resserella obicularia,Leptostrophia elegestica等,以及三叶虫:Encrinurus.红柳沟组为钙质细砂岩、泥质灰岩、生物碎屑灰岩,灰岩中化石十分丰富,含床板珊瑚:Favosites cf.[zhifangensis,Mesofavosites shang-siensis,Hil aepora,Pseudoplasmopora;四射珊瑚:Amsdenoides,Laccophyllumetc.:三叶虫:Encrinurus,Phacops:头足类:Geisonoceras,Michelinoceras等.与白山包组整合接触.苦水泉组整合在红柳沟组之上,为中厚层状凝灰质粉砂岩、细砂岩、沉凝灰岩,夹少量钙质砂岩和砾岩,在下部发现床板珊瑚(Favosites)、四射珊瑚(Petraia,Hapsiphyllum,Syringa-xon)、三叶虫(Encrinurus)、腹足类及放射虫化石.该区中及上志留统可与中国新疆北部、东北、内蒙、蒙古及苏联等地同期地层进行对比.

 
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