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   kunlun 的翻译结果: 查询用时:0.163秒
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kunlun
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  昆仑
     THE FIELD TEST OF THE KUNLUN CF-4 15W/40 DIESEL ENGINE OIL
     昆仑CF-4 15W/40柴油机油行车试验
短句来源
     EA (2-4V, 20-100Hz) was applied to Xuanzhong and Kunlun points for 20min.
     以“悬钟”穴、“昆仑”穴为EA穴位,EA刺激参数选择为2~4V,20~100Hz,20min;
短句来源
     Pb-Sr-Nd-O Isotope Characteristics of Granitoids in East Kunlun Orogenic Belt
     东昆仑造山带花岗岩类Pb-Sr-Nd-O同位素特征
短句来源
     Rupture segmentation and process of the 2001 M_w 7.8 Central Kunlun, China. earthquake
     2001年中国中昆仑M_w7.8级地震的破裂段及破裂过程
短句来源
     K-Ar ages of basic-acid dikes of the 118-323 km section of the Xinjiang-Tibet Highway in the West Kunlun
     西昆仑新藏公路118~323km段基性、酸性岩脉K-Ar年龄
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  昆仑山
     the front zone of the Kunlun Mountains has risen1380m from4.15to1.66Ma BP,with an average uplift rate of0.55mm/a,and risen4140m since1.66Ma BP,with an average uplift rate of2.49mm/a;
     昆仑山前山地带4.15Ma至1.66Ma间总共抬升了1380m,平均抬升速率为0.55mm/a; 1.66Ma以来总共抬升了4140m,平均抬升速率为2.49mm/a。
短句来源
     the rear zone of the Kunlun Mountains has risen1500m from3.85to1.66Ma BP,with an average uplift rate of0.70mm/a,and it has risen5140m since1.66Ma BP,with an average uplift rate of3.19mm/a.
     昆仑山后山地带3.85Ma至1.66Ma间总共抬升量约为1500m,平均抬升速率为0.70mm/a; 1.66Ma以来总共抬升量约为5140m,平均抬升速率为3.19mm/a。
短句来源
     Results The CMS prevalence of army stayed at 4300 m,5100m and 5380m for 1 year in Kala Kunlun mountain was 37.0%,67.9% and 92.9%;
     结果驻喀喇昆仑山海拔4 300,5 100和5 380 m 1年的某部队CMS的患病率依次为37.0%,67.9%和92.9%;
短句来源
     The petrochemical characteristics of the Carboniferous volcanic rocks in the east part of western Kunlun ( SiO 2 between 42.98% and 50.78 %, Na 2O+K 2O from 1.52% to 5.85%, Na 2O/K 2O 1.53~5.86) imply obviously high sodium.
     火山岩岩石化学研究表明 ,西昆仑山东段北缘石炭纪火山岩的SiO2 含量在 42 .98%~ 5 0 .78%之间 ,Na2 O +K2 O在 1.5 2 %~ 5 .85 %之间 ,Na2 O/K2 O为 1.5 3~ 5 .86 ,显示出明显的富钠特征。
短句来源
     SOURCE PROCESS OF THE 14 NOVEMBER 2001 WESTHERN KUNLUN MOUNTAIN M_S8.1 EARTHQUAKE
     2001年11月14日昆仑山口西M_S8.1地震震源破裂过程研究
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  “kunlun”译为未确定词的双语例句
     AN ANALYSIS OF WATER RESOURCE CHARACTERISTICS OF THE RIVERS IN THE NORTHERN SLOPE OF THE KUNLUN MOUNTAINS
     AN ANALYSIS OF WATER RESOURCE CHARACTERISTICS OF THE RIVERS IN THE NORTHERN SLOPE OF THE KUNLUN MOUNTAINS
短句来源
     Southern Margin Strike-Slip Fault Zone of East Kunlun Mountains: An Important Consequence of Intracontinental Deformation
     Southern Margin Strike-Slip Fault Zone of East Kunlun Mountains: An Important Consequence of Intracontinental Deformation
短句来源
     Ultramafic cumulate rock has a Sm-Nd isochron age of 1480± 3 Ma, and the garnet amphibolite closely related to it has an 40Ar-39Ar plateau ages of 881.8±4.7 Ma (garnet) and 852.2±1.0 Ma (amphibole), which respectively represent the timing of spreading and subduction Central Kunlun paleo-ocean limit.
     超镁铁质堆晶岩Sm-Nd等时线年龄为1 480±3Ma, 与之紧密伴生的榴闪岩40Ar/39Ar坪年龄为(881.8±4.7)Ma(石榴石)和(852.2±1.0)Ma(角闪石),分别代表了古昆中洋扩张及俯冲消减的时限。
短句来源
     40Ar/39Ar Age of the Basic Sill Swarms of Two Periods in the Junction Area of Qinling and Kunlun and Its Tectonic Significance
     秦昆结合区两期基性岩墙群~(40)Ar/~(39)Ar定年及其构造意义
短句来源
     The family of poaceae contains 49 genus and 163 species in Kunlun area.
     本区禾本科植物有49属163种。
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  kunlun
The Middle Kunlun fault (F10), which is the main structure of the Kunlun fault zone, is a high angle, super-deep fault.
      
Based on the conductive structure of the profile, the southern part of the Middle Kunlun fault belongs to the Tibetan plateau, but it is not certain whether the northern part of the Middle Kunlun fault belongs to the Tibetan plateau.
      
Three Late Triassic plate sutures, namely, the Longmu Co-Shuanghu suture, Kunlun-Qinling suture and Xijinwulan-Jinshajiang suture, have been recognized on the Qinghai-Tibet plateau.
      
The Kunlun Platform was situated in the south, where there were two small lands.
      
Shuttle imaging radar-C (SIR-C) detection for the Cenozoic volcanoes in West Kunlun, China
      
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This paper deals with the distribution of carbon-dioxide discharging localities in China (where CO2 gas content is >90% and water with dissolved CO2 >1g/l or with bicarbonate more than 1g/l), characteristics of water quality and the seismic activities of various carbon-dioxide discharging zones. The source of CO2 fluids is also studied herein. It is suggested that the highly seismic activities are mostly associated with the zones of warm and hot springs rich in carbon-dioxide, but scarcely with the zones of...

This paper deals with the distribution of carbon-dioxide discharging localities in China (where CO2 gas content is >90% and water with dissolved CO2 >1g/l or with bicarbonate more than 1g/l), characteristics of water quality and the seismic activities of various carbon-dioxide discharging zones. The source of CO2 fluids is also studied herein. It is suggested that the highly seismic activities are mostly associated with the zones of warm and hot springs rich in carbon-dioxide, but scarcely with the zones of cold carbon-dioxide springs. Warm and hot carbon-dioxide springs occur mainly in seis-mically active zones with strong neotectonic movements, such as in southern Xizang (Tibet) where the highly seismic activities are accompanied with regional metamorphism. Moreover, in area of heat flow anomaly probably there also occurred magmatic intrusion which brought about contact metamorphism and through all of these processes carbon-dioxide may be released. Cold carbon-dioxide springs are discharged in seismically less active zones, such as in Northeast China, where tectonic movements and magmatic activities became gradually quiescent. Carbon-dioxide appears to be released slowly from magma which cooled down under a relatively closed condition in the post-volcanic period, and it miaght be the released gases conserved in the altered surrounding rocks affected by volcanic magma. Meanwhile, the cold carbon-dioxide springs originated by mixing CO2 fluid with shallow groundwater.In the seismically active zones within depressions subsides since Cenozoic time, such as in North China, the warm and hot carbon-dioxide springs have not been found at the ground surface, owing to the thick covers, but in the case of deep-seated ground-water hot carbon-dioxide water was discovered. Intensive studies of the origin and distribution of CO2 fluids will be significant to understanding the recent stress field, seis-micity and regional metamorphism. It must be stressed that great effort must be made in the studies of mountainous areas, such as the Kunlun-Szechuan-Yunnan, Tienshan, Chilien. Moreover, the analysis of stable carbon isotopes from discharges of CO2 fluids should also be carried out.

本文举例阐述了我国碳酸水出露点的分布、水质特征及各类型碳酸水出露带的地震活动性,并探讨了二氧化碳的来源。认为深入研究碳酸水成因和分布特征对研究近代构造应力场、地震活动性、现代正在进行着的变质作用等是有意义的。

Studies were carried out in Beijing ( 80m ) , Germu ( 2800m ) and Kunlun Pass (4500-4600 m above sea level) .Altogether, 400 young male nonnative residents, were examined. The items of investigation were as follows: physical examination, electrocardiography,vectorcardiography, cardiac systolic interval, pulmonary rheo-graphy, echocardiography etc. It was demomstrated that they main characteristic features of the left axis deviation and incomplete right bundle-branch block at high altitude were different...

Studies were carried out in Beijing ( 80m ) , Germu ( 2800m ) and Kunlun Pass (4500-4600 m above sea level) .Altogether, 400 young male nonnative residents, were examined. The items of investigation were as follows: physical examination, electrocardiography,vectorcardiography, cardiac systolic interval, pulmonary rheo-graphy, echocardiography etc. It was demomstrated that they main characteristic features of the left axis deviation and incomplete right bundle-branch block at high altitude were different from those observed at sea level, A classification and diagnostic criteria of right ventricular hypertrophy at high altitude were suggested, and the chronic and acute effects of high altitude environment on the right and left heart were discussed.

本文报告高原环境对400例移居高原的男青年心脏影响的研究结果,并提出关于高原右心室肥厚分型方案和诊断标准的建议。各项研究的详细资料将陆续发表。

25 acclimatized young males to Germu(2,800 m. above sea level)were submitted to echocardiographic examination in Kunlun Pass(4,500 m.)one month after arrival,and then in Beijing(80 m.)after residing there for three months. The primary results were as follows.. A slower heart rate, a shorter isometric diastolic interval of right ventricle and a lower pulmonary systolic pressure were found at sea level in comparison with that at high altitude, but there was no statistical difference in transverse diameters...

25 acclimatized young males to Germu(2,800 m. above sea level)were submitted to echocardiographic examination in Kunlun Pass(4,500 m.)one month after arrival,and then in Beijing(80 m.)after residing there for three months. The primary results were as follows.. A slower heart rate, a shorter isometric diastolic interval of right ventricle and a lower pulmonary systolic pressure were found at sea level in comparison with that at high altitude, but there was no statistical difference in transverse diameters of the right ventri-cle, the right ventricular tract and the right pulmonary artery. The stroke volume and the left ventricular end-diastolic volume were greater at sea level. The cardiac index and the ejection fraction showed a downward tendency from Kunlun Pass to Beijing, but the minute volume was practically identical.In addition, we made a comparison of the echocardiogram between two groups at sea level, one of them was those coming from high altitude. Finally, the possible significance of the changes presented above was discussed.

对移居海拔2800米地区半年以上的25例男性青年,在其到达海拔4500米地区一个月后作超声心动图检查;在其回到海拔80米地区定居三个月后又作复查。结果是:海平与高原比较。心率变慢、右室等容舒张期缩短,肺动脉收缩压降低;但右室横径、右室流出道与右肺动脉内径无显著差异。海平每搏量与左室舒张末期容积增大,而心指数与排血分数有降低趋势;但每分心输出量大致相同。另外,比较了高原移居者平原恢复值与平原正常人的对照值。

 
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