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新疆地区
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  xinjiang region
    THE COESEISMIC EFFECT IN XINJIANG REGION WHEN THE M_S7.9 EARTHQUAKE OCCURRED IN THE BOUNDARIES ANOMG RUSSIA,MONGOLIA AND CHINA ON SEP.27,2003
    2003年9月27日俄、中、蒙交界7.9级地震新疆地区的同震效应
短句来源
    Coseismal effect of indonesia M 8.7 earthquake on Dec.26,2004 in Xinjiang region
    2004年12月26日印尼8.7级强震新疆地区的同震效应
短句来源
    The results indicate that (1) Average Pn velocity in Xinjiang region is 8.2 km/s, which is higher than the average 8.0 km/s for the mainland of China. The velocity varies from -0.3 km/s to 0.2km/s.
    主要结果是 :①新疆地区平均Pn速度为 8 2km s ,高于中国大陆地区的平均值 (8 0km s) ,速度变化量从 - 0 3km s到 0 2km s.
短句来源
    In the study, we collected 1156 broadband vertical components recorded at 22 digital network stations in Xinjiang region, rümqi station, and 7 stations in the adjacent regions during the period of 1999~2003. The records were firstly processed by the stacked spectral ratio method to obtain Q 0 ( Q at 1 Hz) and the frequency correlation factor η corresponding to each path.
    首先运用叠加谱比法, 对新疆地区22个数字化台网台站、乌鲁木齐台站以及周边的7个台站1999~2003年上半年所记录的1 156个宽带垂直记录, 进行了处理, 得到了与各射线相对应的Q0 值(1 Hz处的Q值)和频率相关因子η.
短句来源
    Based on the results, the distribution images of Q 0 and η in 1°×1° grids for Xinjiang region were gained by the back projection technique.
    在此基础上, 应用反投影技术, 得到了新疆地区1°×1°网格的Q0 值和η值的分布图象.
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  xinjiang area
    STATISTICAL ANALYSIS OF EARTHQUAKES IN XINJIANG AREA
    新疆地区地震发生的统计分析
短句来源
    Theory of Informational Forecast and M_ s≥7 Strong Earthquake Trend in Xinjiang Area
    信息预测理论与新疆地区7级强震趋势研究
短句来源
    VARIATION OF GRAVITY FIELD OF XINJIANG AREA AND JIASHI M_S6.8 EARTHQUAKE
    新疆地区重力变化与伽师6.8级地震
短句来源
    An effective approach for imminent tracing of seismic risk region ——Application of CO_2 observation in Xinjiang area
    地震危险区短临跟踪的一种有效观测手段——地下岩土气体CO_2观测在新疆地区的应用
短句来源
    Based on the informational forecast theory of Weng Wenbo, we discuss the temporal orderliness and commensurability and its web structure of M s≥7 strong earthquakes in Xinjiang area. The major periods of 41a,30a(60a,90a), 11-12a in activity of strong earthquakes in this area possess very important significance.
    简要介绍了翁文波信息预测理论 ,据此对新疆地区 7级强震活动的有序性、可公度性及其网络结构进行了分析研究 ,并指出本区 7级强震活动所呈现的多个有序周期中 4 1a、30a(6 0a、90a)、11a具有特别重要的预测意义 .
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  “新疆地区”译为未确定词的双语例句
    Seismic hazard analysis results of 79 cities in Xinjiang are presented, and the bedrock peak ground accelerations under three seismic levels and their ratios are discussed, and then the relationship between earthquake environments and the seismic hazard analysis results of different exceeding probabilities have been researched.
    通过分析新疆79个城市的地震危险性,获得了新疆地区50年超越概率63%(小震)、10%(中震)、2%(大震)的基岩峰值加速度及其相互比值,研究了地震环境与不同概率地震危险性分析结果之间的关系。
短句来源
    STUDY OF REGIONAL VARIATIONS OF Lg CODA Q IN XINJIANG USING STACK SPECTRAL RATION METHOD
    用叠加谱比法研究新疆地区Lg尾波Q值的区域性变化
短句来源
    The Preliminary Application of S-Wave Splitting in Xinjiang
    S波分裂在新疆地区的初步应用研究
短句来源
    According to the historical recordings of earthquakes in Xinjiang since this century,the author analyzed the earthquake occurrence patterns,making 5. 5, 6. 0, 6. 5, 6 , 7. 0, 7.2 the lower bounds of magnitude and each group of data the update processing samples. Statistical examination showed that earthquakes with different magnitude limitation can be regarded as Poisson process.
    根据新疆地区本世纪的地震记载,分别取5.5、6.0、6.5、6、7.0、7.2为震级下限,视各组资料为更新过程的样本、分析地震发生的统计特征.经统计检验,不同震级下限的地震发生皆可认为是泊松过程;
短句来源
    Two parameters, σ N and σ E,depicting the calming and clustering of seismicity anomalies in medium and short term before strong earthquakes are calculated in Xinjiang earthquake regions from 1970~1998(the window length is 1 year and the step length is 3 months).
    利用2 个描述强震前中短期阶段地震活动异常平静及丛集的参量,计算了新疆地震区1970~1998 年以1 年为窗长、3 个月为步长的地震活动异常图像,并给出了发生在新疆乌恰的2 次7.4 级地震前后,新疆地区σN 异常分布动态演化图像。
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  xinjiang region
(2) The affected areas of dust storms can be divided into seven sub-regions, that is, North Xinjiang Region, South Xinjiang Region, Hexi Region, Qaidam Basin Region, Hetao Region, Northeastern China Region and Qinghai-Xizang (Tibet) Region.
      
The area of the most frequent occurrence of dust storms and floating-dust is in South Xinjiang Region, and of wind-blown sand in the Hexi Region.
      
The maximum interannual change and variance of dust events during this time happened in South Xinjiang Region and Hexi Region.
      
However, in South Xinjiang Region and North Xinjiang Region, which was less affected by monsoon climate, dust events may occur at any time of the year, less than 50% of the events in this region occur during spring.
      
The total rare-earth element values (ΣREE) of loess in the Xinjiang region vary over a range of 128-200 ppm, with an average of 153 ppm.
      
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  xinjiang area
As a consequence of global warming and an enhanced water cycle, the climate changed in northwest China, most notably in the Xinjiang area in the year 1987.
      


A model for estimating evaporation have been tested by using hydrological and meteorological data in Xinjiang. It is shown that the model can be used to estimate normal year evaporation of the basin from the monthly observations of meteorogieal station, and with satisfactory accuracy. It is also found that the model introduced in this paper is suited to inland area in northwest China.

本文利用新疆地区的水文气象资料检验了一个计算蒸发量的模式。结果表明该模式有较满意的精度,可用于根据气象资料计算流域的蒸发量,在我国西北内陆地区有较强的适应性。

Xinjiang has the number of glaciers of 19374, and area of 25458.4km~2, and the storangeof ice about 26831 ×108m~3. The watery stouage of glaciers in Xinjiang is about 29 times asmuch as the amount of the surface runoff, and supplies about 196×10~8 m~3 per year, and is thesource of agriculture irrigation to some oases. The large number of and large scale of glaciersin Xinjiang is richly endowed by natural resources. Its commercial value is different in variousarea. Among them, the commercial value of glacier...

Xinjiang has the number of glaciers of 19374, and area of 25458.4km~2, and the storangeof ice about 26831 ×108m~3. The watery stouage of glaciers in Xinjiang is about 29 times asmuch as the amount of the surface runoff, and supplies about 196×10~8 m~3 per year, and is thesource of agriculture irrigation to some oases. The large number of and large scale of glaciersin Xinjiang is richly endowed by natural resources. Its commercial value is different in variousarea. Among them, the commercial value of glacier resource in western area of Tarim basin isthe highest.

根据最新冰川编目资料,统计了新疆地区的冰川,共19374条,冰川面积25458.4km~2;分析了分布特征,具有自北而南和自东而西的差异;讨论了新疆冰川的资源意义,其经济价值的大小因地而异。

This paper presents the computing formula and method of general information fractal and studiesNorth China, Southern Yellow Sea and its cast, Sichuan-Yunnan, Gansu-Qinghai-Ningxia, andXinjiang areas where there are more earthquakes except Qingzang highland where the metworks of stations are quite few and have no observational ability for moderate and small earthquakes, The resultshows that there is a relatively obvious fractal drop process before some main earthquakes;there are certain fractal drop anomalies...

This paper presents the computing formula and method of general information fractal and studiesNorth China, Southern Yellow Sea and its cast, Sichuan-Yunnan, Gansu-Qinghai-Ningxia, andXinjiang areas where there are more earthquakes except Qingzang highland where the metworks of stations are quite few and have no observational ability for moderate and small earthquakes, The resultshows that there is a relatively obvious fractal drop process before some main earthquakes;there are certain fractal drop anomalies before some moderately strong earthquakes in North China areal there areobvious fractal drops after strong earthquakes in high scale value areas of spatial information fractal inXinjiang, Gansu-Qinghai -Ningxia regions, but there are no fractal drops before earthquakes, thereare precursory fractal drops before earthquakes in all low scale value areas and they recovered afterearthquakes. The precursory drop of time fractal is more obvious than spatial fractal. When tested byXu's R value, Rs= 0. 386, Rt= 0. 83, all exceeding the marked level.

给出了广义信息维的计算公式和方法,对中国大陆除青藏高原由于台网太稀,对中小地震无监控能力未作计算之外,对其余地震较多的华北、南黄海及其沿岸、川滇、甘青宁、新疆地区都进行了研究。结果表明,在一些主要地震前,都有一个较明显的降维过程,在华北地区一些中强震之前,也有一定的降维异常。在新疆,甘青宁地区的空间信息维高标度值区在强震发生之后有明显的降维,而在震前没有,低标度值区在震前都有前兆性降维,而震后恢复。时间分维的前兆性降维比空间分维明显。用许氏R值进行检验,R=0.386,Rt=0.83,均超过显著水平。

 
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