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长城
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  great wall
     Values of gravity datum points and accuracy obtained at Great Wall Station are 982208.682 and ±0.021 mgal respectively.
     测得长城站重力基准点重力值及精度为:982208.682±0.021mgal.
短句来源
     Communication of ARL 8680 XRF Spectrometer with Great Wall 0520-CH computer
     8680 X荧光光谱仪与长城0520-CH计算机的数据通信
短句来源
     Results show that there are large cloud and aerosol optical depths with mean values of 12.7 and 0.094, respecively, during summer at the Great Wall Station.
     结果表明,在长城站夏季,云和气溶胶的光学厚度都较大,其均值分别为12.7和0.094。
短句来源
     Ionograms and magnetograms at Great Wall (62°13′S,58°58′W),Antarctica,were used to study the sub auroral ionospheric effects of the March 13,1989 magnetic storm.
     利用南极长城站(62°13′S,58°58′W)频高图和磁照图研究了1989年3月13日磁暴的亚极光区电离层效应。
短句来源
     Application Of Great Wall Brand 15W/40 CF-4 Diesel Engine Oil In High Speed Diesel Buses
     长城15W/40 CF-4柴油机油在高速柴油车上的应用
短句来源
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  the great wall
     Results show that there are large cloud and aerosol optical depths with mean values of 12.7 and 0.094, respecively, during summer at the Great Wall Station.
     结果表明,在长城站夏季,云和气溶胶的光学厚度都较大,其均值分别为12.7和0.094。
短句来源
     In this paper, a neutron activation analysis was used to determine trace elements in the surface sediments of the Great wall Bay, Antarctica. The contents of 28 elements were given quantitatively. These elements are Au, Ag, La, Ce, Nd, Sm, Eu, Tb, Yb, Lu, U, Th, Cr, Ir, Zr, Hf, Ba, Sr, Cs, Ni, Sc, Rb, Zn, Ta, Co, As, Sb, and W.
     本文采用中子活化分析法测定了南极长城湾表层沉积物中的微量元素,定量地给出了Au、Ag、La、Ce、Nd、Sm、Eu、Tb、Yb、Lu、U、Th、Cr、Ir、Zr、Hf、Ba、Sr、Cs、Ni、Sc、Rb、Zn、Ta、Co、As、Sb、W等28种元素的含量,测定不准确度为3~5%。
短句来源
     Investigation of the Great wall for Ecology in Northern China
     中国北方长城的生态学考察
短句来源
     This paper reports the analysis results (including pH, conductivity and ion concentrations) of the precipitation samples collected at the Great Wall Station of Antarctic(62°13′S, 58°58′W, ASL 10.0 m) in 1998. The average pH value and conductivity are 5.62 and 85.16 μS/cm,respectively.
     文中报告了 1998年 1~ 12月 ,在中国南极长城站 (6 2°13′S ,5 8°5 8′W ,海拔 10 .0m)采集的 115个有效降水样品的 pH值、电导率和化学组分分析结果。 长城站地区降水的年平均 pH值为 5 .6 2 ,电导率年平均值为 85 .16 μS/cm。
短句来源
     Influence and Vicissitude of Communication of Economical Cultures in the Zone of the Great Wall
     长城带经济文化交流的影响与变迁
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  “长城”译为未确定词的双语例句
     B. spinifera,C.
     在长城湾,B. spinifera, C.
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     The 12%Cr type steels- 1Cr12Mo and 2Cr12NiMo1W1V for turbine blades have been pilot produced by 30 t EAF+VOD-ESR(2~3 t ingot)-825mm mill at Changcheng Special Steel.
     长城特钢采用 30tEAF +VOD ESR(2~ 3t锭 ) 82 5mm轧机试生产了 1Cr12Mo ,2Cr12NiMo1W 1V等 12 %Cr型叶片用钢。
短句来源
     The Display Structure of GW0520CH—014 Board
     长城0520CH—014板的显示结构
短句来源
     Communication between GreatWall 0530 and M-340S Computer
     长城0530与M—340S中型机联机通讯
短句来源
     The optimum concentration of Lan-826, Changcheng 3 # and Ruoding was 0.3%, 0.3% and 0.4% respectively.
     兰 82 6和长城 3# 的最佳添加量在 0 .3% ,若丁为 0 .4%。
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  great wall
Research on plate motion, crustal movement, orbit determination, and atmospheric monitoring, including the ionosphere and troposphere, were performed using GPS data of the Great Wall Station, Zhongshan Station and Yellow River Station.
      
During the 2004/2005 austral summer season, the absolute gravity and relative gravity were measured at the Great Wall Station with precision within ± 3 × 10-8 ms-2 and ± 10 × 10-8 ms-2 respectively.
      
Determination of trans-Resveratrol in China Great Wall ''Fazenda'' Red Wine by Use of Micellar Electrokinetic Chromatography
      
When resveratrol was determined in the top-grade dry-red wine China Great Wall ''Fazenda'' by use of our analytical method the concentration was found to be ≥1.3 ± 0.1 mg L-1.
      
The Archaeology of the Great Wall of the Qin and Han Dynasties
      
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  the great wall
Research on plate motion, crustal movement, orbit determination, and atmospheric monitoring, including the ionosphere and troposphere, were performed using GPS data of the Great Wall Station, Zhongshan Station and Yellow River Station.
      
During the 2004/2005 austral summer season, the absolute gravity and relative gravity were measured at the Great Wall Station with precision within ± 3 × 10-8 ms-2 and ± 10 × 10-8 ms-2 respectively.
      
The Archaeology of the Great Wall of the Qin and Han Dynasties
      
This paper traces the routes of the entire length of the Great Wall along China's northern border in the Qin and Western Han Dynasties.
      
PIPER RAE GAUBATZ, Beyond the Great Wall: Urban Form and Transformations on the Chinese Frontiers, Stanford: Stanford University
      
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This paper discusses the line of demarcation of Palearctic and Oriental Regions onthe basis of the data of the distribution of some agricultural insects east of Chinling.This article is divided into 4 parts: The first part summarizes the different opinions of Chinese and foreign scholars onthe location of the line. In the second part, the writer listed 194 species of agricultural insects belonging tothe Palearctic and Oriental faunae as circumscribed by the natural lines of Great Wall,Yellow River, Hwai Ho,...

This paper discusses the line of demarcation of Palearctic and Oriental Regions onthe basis of the data of the distribution of some agricultural insects east of Chinling.This article is divided into 4 parts: The first part summarizes the different opinions of Chinese and foreign scholars onthe location of the line. In the second part, the writer listed 194 species of agricultural insects belonging tothe Palearctic and Oriental faunae as circumscribed by the natural lines of Great Wall,Yellow River, Hwai Ho, Yangtze River and Nanling Mountains, to the east of Chinling. The third part discusses the insect faunae of Honan and Hupeh on the basis of thiscomparison, the author suggest that the line should be drawn to the south of Hwai Ho,and thus Nanyang (南阳) and Sinyang (信阳) districts of Honan Province should beconsidered to be in the Oriental Region. In the fourth part, it is stated that according to the analysis of the composition of theagricultural insects of Yangchow, Nanking, Hanchow and Wenchow, the line in Kiangsuand Chekiang Provinces should be drawn along the north side of the Yangtze River. The line of the two above regions in Anhwei Province has not been fully discusseddue to lack of sufficient reference, but it seems to be between the Hwai Ho and YangtzeRiver, probably somewhere north of Hofei (合肥) according to the known data.

本文系以某些主要农业害虫的分布资料为依据,来讨论古北、东洋两地区在我国秦岭以东的分界线问题。 全文分为四个部分,第一部分着重介绍中外学者对于这条界线摆法的几种不同意见。第二部分将194种农业昆虫在我国秦岭以东的交杂渗透情况,依长城、黄河、淮河、长江、南岭等五条界线,列举它们分布区(或为害区)的南限或北限。第三部分讨论了古北、东洋两地区在豫鄂一带的分界线,提出应摆在淮河以南,即将河南南部的南阳盆地及信阳专区,亦划入东洋区中。第四部分进一步讨论了两地区在江、浙一带的分界线问题,则主张划在长江北岸,比较妥当。

In the light of the recent geological informations and field observations on the Sinian stratigraphical subdivisions and structural framework in South China the present authors are led to the conclusion that the lower boundary of the Sinian sequence should be shifted downwards. The newly established scheme of the Sinian stratigraphical subdivisions of southern China from base upward consists of Szepao series, Panhsi series, Puling series and Chiatung series. Based on the study of the type section of the Chihsien...

In the light of the recent geological informations and field observations on the Sinian stratigraphical subdivisions and structural framework in South China the present authors are led to the conclusion that the lower boundary of the Sinian sequence should be shifted downwards. The newly established scheme of the Sinian stratigraphical subdivisions of southern China from base upward consists of Szepao series, Panhsi series, Puling series and Chiatung series. Based on the study of the type section of the Chihsien area in North China, the Szepao series, Panhsi series and Puling series of South China can be correlated respectively with the Changcheng series, Chihsien series and Chingpeikou series of North China, while a stratigraphical hiatus usually exists betweer the Sinian and the Cambrian which marks the Chihsienian movement in the Chihsien area and thus the Chiatung series is not represented in North China. The large amounts of the Sinian andesitic volcanic rocks and the extensively distributed and developed Sinian flysch formation suggest the existence of an ancient volcanic arc-trench system occurring within the area of the Kiangnan geanticline and its southeastern side during the Sinian period.

华南震旦系下限应下移,包括上下板溪群和与其相当的地层。自下而上可分为“四堡统”、“板溪统”、“铺岭统”和“峡东统”四个统。以蓟县震旦系剖面为我国震旦系标准,南北方震旦系可以对比,南方的下面三个统分别与蓟县剖面的长城统、蓟县统、青白口统相当,“峡东统”在蓟县地区缺失。震旦纪在江南地背斜范围内形成过古岛弧,并有古海沟的发育。

In this report some evidences of ancient earthquakes found in the North China region are presented as follows.1. the ruins of ancient cities in the Hang dynasty distracted by the earthquakes having occurred in the area northwest of Dengkou County, Nei Monggol Autonomous Region; 2. The offset of Great Wall and fault scarps by the ancient earthquakes in Hungguozigou area northwest of Pinglo County, Ningxia Autonomous Region; 3. The paleoseismic faults and liquefaction and deformation of sandy ground in Guchenzi...

In this report some evidences of ancient earthquakes found in the North China region are presented as follows.1. the ruins of ancient cities in the Hang dynasty distracted by the earthquakes having occurred in the area northwest of Dengkou County, Nei Monggol Autonomous Region; 2. The offset of Great Wall and fault scarps by the ancient earthquakes in Hungguozigou area northwest of Pinglo County, Ningxia Autonomous Region; 3. The paleoseismic faults and liquefaction and deformation of sandy ground in Guchenzi area, Zhongning County, Ningxia Region; 4. Landslide zones in loess caused by the ancient earthquakes in the Tianshui-Baoji-Changxing region; 5. Seismic fissures and rock falls in Haicheng County, Liaoning province; 6. The folds and deformation of lacustrine diatomite layer by earthquakes in Lingqu County, Shandong province; 7. Paleoseismic fissures in Xingyi County, Jiangsu province. These results are of significance in regional seismic evaluation.

本文简要报导华北地区几个古地震实例:1.内蒙磴口西北地震毁坏的汉代古城废墟;2.宁夏平罗西北红果子沟长城错开及古地震断层陡坎;3.宁夏中宁古城子古地震断层及沙基液化变形;4.天水—宝鸡—常兴古地震黄土滑坡带;5.辽宁海城黑音寺山地震裂缝及岩崩;6. 山东临朐山旺湖相硅藻土层中地震引起的揉皱变形;7.江苏新沂嶂山闸古地震裂缝。

 
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