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新疆阿尔泰山
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  “新疆阿尔泰山”译为未确定词的双语例句
     One newly recorded genus to China, Rhammatophyllum O.
     报道了采自新疆阿尔泰山地区的1个中国新记录属假糖芥属Rhammatophyllum O.
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     Based on studying the bryophytes in Altay Mountains,Xinjiang,three new records from Xinjiang are reported,they are Brachythecium pseudo-subalbicans Y.
     通过对新疆阿尔泰山苔藓植物的调查研究,发现新疆新纪录种3种,分别为:亚灰白青藓Brachythecium pseudo-subalbicans Y.
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     By studying the ages of valley terraces of 26 rivers at Altai Mountain, West Jungeer Mountain,southern and northern Tianshan, and Kunlun Mountain, it is indicated that high alluvial flats were mainly formed in 3 000 aB.P.
     对新疆阿尔泰山、西准噶尔山地、天山南北及昆仑山26 条河流河谷阶地的年代学研究表明:高河漫滩主要形成于晚全新世时期3 000 aB.P.;
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     New understanding on origin of Kalaxiangeer copper deposit on southern margin of Altay mountain, Xinjiang: Constraints from S-Pb-H-O isotope geochemistry and ~(40)Ar-~(39)Ar age of Halasu copper deposit
     新疆阿尔泰山南缘卡拉先格尔斑岩铜矿带成因再认识——来自哈腊苏铜矿硫-铅-氢-氧同位素和~(40)Ar-_~(39)Ar年龄的约束
短句来源
     It is controlled by NW trend faults. There are three kinds of mineralizing hydrothermal alternation: silicate, skarnization and chloritization. The silicified ores are characterized by high contents of SiO 2 and Fe 2O 3+FeO, while skarnized ores by high contents of CaO and Al 2O 3. Different ores are rich in Au, Ag, Cu, Pb, Zn, Bi, Mo, W elements.
     萨热阔布金矿床位于新疆阿尔泰山南缘泥盆系康布铁堡组火山碎屑岩中 ,受断裂控制 ,成矿热液蚀变以硅化、似夕卡岩化、绿泥石化为主 ,硅化蚀变矿石富Fe2 O3+FeO、SiO2 ,而似夕卡岩蚀变矿石富CaO和Al2 O3,各种矿石富集Au、Ag、Cu、Pb、Zn、Bi、Mo、W等多种元素。
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  相似匹配句对
     A PRELIMINARY INSPECTION ON THE ELK(ALCES ALCES)IN XINJIANG ALTAI MOUNTAIN
     新疆阿尔泰山驼鹿的初步考察
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     Taxonomic Classification ofthe Soilsin The Altay Mountains
     新疆阿尔泰山土壤系统分类
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     Rock Paintings in Xinjiang
     新疆岩画
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     FLICKERING XINJIANG
     舞动的新疆
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     THE ACTIVE FAULTS IN ALTAI MOUNTAINS
     阿尔泰山活动断裂
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Chemical analysis, EPMA, optical absorption, X-ray topography, IR and Mssbauer spectroscopy were conducted on colour-banding tourmaline from Altai granitic pegmatite, Xinjiang, to investigate the mechanism of its colour change. Altai tourmaline usually has a red core enveloped by green rings. It has been observed by means of X-ray. topography that change in colour is always accompanied by abrupt change in texture.The core shows macromasaic texture but the outer rings are of lamellar texture. Optical absorption...

Chemical analysis, EPMA, optical absorption, X-ray topography, IR and Mssbauer spectroscopy were conducted on colour-banding tourmaline from Altai granitic pegmatite, Xinjiang, to investigate the mechanism of its colour change. Altai tourmaline usually has a red core enveloped by green rings. It has been observed by means of X-ray. topography that change in colour is always accompanied by abrupt change in texture.The core shows macromasaic texture but the outer rings are of lamellar texture. Optical absorption and EPMA results suggest that the difference in colour can be related to the slight variation in iron and manganese. Iron increases, while manganese decreases from the core to the outer area of the crystal. Therefore, the formation of colour bands can be attributed to the changing growth condition. According to the distribution features and homogenization temperatures of fluid inclusions in tourmaline, it can be concluded that there are two distinct growth stages separated by partial dissolution in hydrothermal process.

本文以新疆阿尔泰山地区花岗伟晶岩中的色带电气石为重点,应用X射线透射形貌技术,揭示了光学显微镜无法查明的结构缺陷,结合晶体表面微形貌观察及包裹体研究,阐明了色带电气石晶体的形成过程和生长机理。同时运用吸收光谱、穆斯鲍尔谱、红外吸收、核磁共振等谱学方法,对照光谱及化学分析、电子探针分析结果,对阿尔泰不同颜色的电气石晶体,特别是玫瑰色的颜色起因作了较全面的讨论。

Based on macroscopic and microscopic research analysis of the fluid inclusions and Study of the geological charactristics the authors are under the impression that the granitic batholiths in Southern Altay Mountains Xinjiang Autonomous Region are S—type granites They belong to semi-autochthonous remelting migmatitic granites whice extend along the axis of laegr regional anticlinorium The diagenetic perssure is above 1.1kb and the temperature is above 416℃.

通过对新疆阿尔泰山南缘原划为侵入的花岗岩基进行深入的,从宏观到微观的观察、研究后认为应属于 S 型花岗岩.根据岩石包裹体测试结果,求得成岩压力大于101×10~8 pa,温度大于416℃.结合地质特征,属于沿区域上大的复式背斜轴部分布的重熔型半原地混合花岗岩.

Based on the Quaternary glacial remains and their characteristics in the Halasi River catchment and its surroundings in the Altai Mountains in Xingjiang of China. It was found that there existed five ancient glaciated stages during Quaternary period. They are the third Glacial Stage, the second Glacial Stage and the Last Glacial Stage in pleistocene, and Neoglaciation and Little Ice Age in Hdocene. The three pleistocene glaciations had a massive scale with ice-capped glaciers. During the third Glacial Stage...

Based on the Quaternary glacial remains and their characteristics in the Halasi River catchment and its surroundings in the Altai Mountains in Xingjiang of China. It was found that there existed five ancient glaciated stages during Quaternary period. They are the third Glacial Stage, the second Glacial Stage and the Last Glacial Stage in pleistocene, and Neoglaciation and Little Ice Age in Hdocene. The three pleistocene glaciations had a massive scale with ice-capped glaciers. During the third Glacial Stage the main valley was fully occupied by the glaciers with the altitade range from 1 900 m to 2 200 m. The large valley glaciers with the length more than 96 km developed during the second and the Last Glacial Stage. The plaistocene glaciers belonged to temperate type with high ice temperature, the great activity and strong erosion. From the old ice stage to new one, the snowline rose higher and higher.

根据新疆阿尔泰山哈纳斯河流域及其邻域第四纪冰川遗迹的类型和特征,哈纳斯河流域第四纪时期至少发生过5次明显的冰川事件,即倒数第三冰期,倒数第二冰期,倒数第一冰期(末次冰期),新冰期和小冰期。其中,更新世的3次冰川作用规模巨大,倒数第三冰期的冰川呈半覆盖式,倒数第二冰期和倒数第一冰期时发育了长达96km以上的大型山谷冰川。古冰川属于冰温高、活动性大和侵蚀能力强的温冰川。从新到老,每次冰期的雪线下降幅度一次比一次大。

 
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