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earthquake of
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  地震
     THE SHAN-TAN EARTHQUAKE OF FEBRUARY 11, 1954
     1954年2月11日甘肃省山丹县的地震
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     ON THE SHENSI EARTHQUAKE OF JANUARY 23, 1556.
     1556年1月23日关中大地震
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     ESTIMATION OF EARTHQUAKE TENDENCY AFTER THE 1967 EARTHQUAKE OF LUHO DISTRICT BY RELATIVE MOTION OF THE EARTH CRUST
     由地壳的相对运动估计1967年炉霍地震后该地区的地震趋势
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     ON THE FRACTURE ZONES OF CHANGMA (昌马) EARTHQUAKE OF 1932 AND THEIR CAUSES
     1932年昌马地震破裂带及其形成原因的初步探讨
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     VARIATION OF AVERAGE DISLOCATION VALUES BEFORE AND AFTER THE HAICHENG(海城) EARTHQUAKE OF FEBRUARY, 1975
     1975年2月海城大地震前后的平均断错变化
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  级地震
     2. XiuYan earthquake of M_L=4.0 occured after various parameters display anomaly of 1—3 months at T=150min when T=9—350min, and Dalian Shock of M_L=4.5 Occured after parameters of T=75min show anomaly of 4—9 months.
     2,在T=9~350min中T=150min的各参量出现异常1~3个月后,发生了岫岩哨子河M_L=4.0级地震,周期T=75min的各参量出现异常4~9个月后发生了大连老铁山M_L 4.5级地震
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     The results show that the anomaly of quartz tilt meter at Yantai station was related to the earthquake of magnitude Ms 4.5 occurred in 122°45' E, 38°10' N, at 0: 29 on December 31, 1993.
     其结果给出,烟台石英倾斜仪异常与1993年12月31日0时29分在东经122°45’,北纬38°10’的Ms4.5级地震有关。
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     Outline of the Earthquake of M 6.9 Occurring in Algeria on May 22,2003
     2003年5月22日阿尔及利亚6.9级地震概述
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     ON OCTOBER 2,1993 RUOQIANG EARTHQUAKE OF MAGNITUDE 6.6
     1993年10月2日若羌6.6级地震
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     THE 1983 HEZE EARTHQUAKE OF MAGNITUDE 5.9
     1983年菏泽5.9级地震
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  “earthquake of”译为未确定词的双语例句
     Short term and imminent anomalies of earthquake of load and unload response ratio of the well level to earth tides
     Short-term and imminent anomalies of earthquake of load and unload response ratio of the well level to earth tides
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     Temporal variations of coda Q ̄(-1) associated with the dahaituoshan, Beijing, earthquake of 1990
     Temporal variations of coda Q~(-1) associated with the dahaituoshan, Beijing, earthquake of 1990
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     The source rupture feature of the southern Taiwan Straits earthquake of September 16, 1994 (Ms7. 3) & the analysis of earthquake circumstance in southeastern coast of China
     The source rupture feature of the southern Taiwan Straits earthquake of September 16,1994 (Ms7.3) & the analysis of earthquake circumstance in southeastern coast of China
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     The Impending Prediction of the Strong Earthquake of M 7.5 Occurring in Taiwan on March 31,2002
     关于2002年3月31日台湾M7.5强震的临震预报
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     Analysis of the Coseismic Effects on Jiangsu Province of the M8.7, Indonesia, Earthquake of Dec.26, 2004
     2004年12月26日印尼8.7级强震后江苏地区同震效应分析
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  earthquake of
These researches also concern differential settlements of Arrow Tower and resistance to earthquake of these historical architecture heritages.
      
The paper describes brackish-water areas of Del'fin Bay and provides quantitative characteristics of macrobenthos communities in these areas considering changes that took place after the lowering of the island and a result of the earthquake of 1994.
      
Spatial and time variations in the critical frequencies foF2 before the strong earthquake of August 15, 1963, with the magnitude M = 7.75 are analyzed.
      
The Racha earthquake of 1991 was the strongest of the earthquakes recorded in the Caucasus.
      
Nonlinear soil behavior during the Chi-Chi (Taiwan) earthquake of 1999 from data of the Dahan vertical array
      
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On 1932 December 25, a destructive earthquake of magnitude 7.6 occurred in the region of Changma, Kansu corridor. In the meizoseismal area, there appeared a large number of fissures and fractures, consisting of types of tension, compression and shear. In this paper, the authors analyse the forms and conditions of producing different kinds of fractures associated with the characteristics of regional tectonics, and then, propose a tentative pattern of field stress related to the seismogenesis for the present...

On 1932 December 25, a destructive earthquake of magnitude 7.6 occurred in the region of Changma, Kansu corridor. In the meizoseismal area, there appeared a large number of fissures and fractures, consisting of types of tension, compression and shear. In this paper, the authors analyse the forms and conditions of producing different kinds of fractures associated with the characteristics of regional tectonics, and then, propose a tentative pattern of field stress related to the seismogenesis for the present earthquake.This seismic event was principally due to the nearly north-south horizontal com-pressional force, which had long been dominating this region since the time of Cretaceous. The new seismic fractural zones appeared nearly coincided with the active area of Changma tectonic faulting. Therefore, it may be concluded that the present earthquake was an episode in the long term of Changma faulting movement.

1932年12月25日,我国甘肃省西部玉门镇以南的昌马地区发生了7.6级地震。震中区产生了规模较大的地面破裂带,其中有张性、压性和剪切等多种型式裂缝。本文根据分析各种自然破坏现象的形成条件,结合极震区地质构造特征,对震源区的应力作用和地震成因提出初步看法。 对地震破裂带的分析结果表明,这次地震起主要作用的是南北向的水平挤压作用,并与自白垩纪以来控制着本区构造断裂的区域应力场是一致的。地震破裂带出现的部位与长期活动的昌马构造断裂带一致。因此,我们认为昌马地震的发生是昌马构造断裂带继承性活动的结果。

Using the results from the analysis of the Keping earthquake of 6.2 magnitude (Richter scale) in western Sinkiang in 16 January 1972, a further study of the seis-mic activities for a larger region around Keping is made. The characteristics of seis-micity, source mechanisms, velocity variations, as well as tectonic movements of the region are correlated and analyzed. Basing upon the results obtained a preliminary discussion of the trend of seismic activities in the region is attempted.

本文通过对1972年1月16日新疆西部柯坪地区6.2级的地震进行重点分析和总结,进一步扩大了研究地区,并从地震活动特征、发震的物理机制、波速变化以及当前的地壳运动等方面进行对比分析,对该地区地震趋势进行了初步探讨。

In this paper, analytical expressions for the earthquake displacement field pro-duced by rectangular strike-slip and dip-slip faults of arbitrary dip in a semi-infinite elastic medium for the case of unequal Lame constants are given in closed forms. Some numerical examples are presented to illustrate the effects of Poisson ratio of the medium, the dip angle, upper and lower boundary of the fault, to earthquake dis-placement field on surface. By comparing the geodetic data of the 1966 Hsingtai earth-quake...

In this paper, analytical expressions for the earthquake displacement field pro-duced by rectangular strike-slip and dip-slip faults of arbitrary dip in a semi-infinite elastic medium for the case of unequal Lame constants are given in closed forms. Some numerical examples are presented to illustrate the effects of Poisson ratio of the medium, the dip angle, upper and lower boundary of the fault, to earthquake dis-placement field on surface. By comparing the geodetic data of the 1966 Hsingtai earth-quake to the theoretical surface displacements that would be produced by a single rectangular slip fault of various strike, dip direction, dip angle, fault length, width, focal depth, and dislocations, it is shown that the simplified single slip fault model can not explain satisfactorily the observed horizontal and vertical ground deforma-tion. In order to account for the observed data, a compounded fault model which consists of six simple rectangular slip faults, is proposed. By using the grid trial method, the source parameters appropriate to the observed horizontal as well as ver-tical displacement field are obtained. The results are as follows: the upper three simple rectangular slip faults breaking to the surface, have a dip angle of 45°, width 15 km, while the lower three simple rectangular slip faults have a dip angle of 82°, width 30 km. Other source parameters determined are as follows: strike, N35°B; dip direction, N125°E; total fault length, 50 km; average strike-slip dislocations respectively, -78, -134, -17, 2, -3, and 1 cm (minus stands for the right-lateral strike-slip while plus for the left-lateral strike-slip); average dip-slip dislocations respectively, 2, 50, 88, 24, -5, and -23 cm (minus stands for the reverse fault while plus for the normal fault); seismic moments respectively, 3.2, 5.9, 3.7, 2.0, 0.5, and 1.9 X 1025 dyne · cm, stress drops respectively, 22, 42, 33, 5, 1, and 4 bars, strain drops respectively, 3.3, 6.4, 5.0, 0.8, 0.2, and 0.6 X 10-5. Lower limit of strain energy release is 6.1 X 1022 ergs. A comparison of the obtained results with the epicentral distri-bution of earthquakes of magnitudes greater than 6 indicates that, the main shock and two larger foreshocks are related more closely with the dislocation of the upper three portions of this compounded fault, and that the two larger aftershocks are related with the dislocation near the ends of the lower portions of this compounded fault. Results of leveling survey in Hsingtai area since 1920, indicate that the upper limit of the rate of subsidence is about 5 mm/yr. If the strain accumulated in this area is as-sumed to be released entirely by the 1966 Hsingtai earthquake, the lower limit of the recurrence period of earthquakes of magnitudes as high as the 1966 Hsingtai earth-quake can be estimated in terms of the average dip-slip dislocation of this compound-ed fault to be about 176 years.

本文以完整的形式给出拉梅常数不相等情形的半无限弹性介质中任意倾角的矩形滑动断层引起的地震位移场解析表示式。以一些数值结果说明介质的泊松比、断层面的倾角、上界和下界对地面的地震位移场的影响。在比较1966年邢台地震的地形变资料和计算得到的各种走向、倾向、倾角、断层面长度、宽度、震源深度和错距的单个的矩形滑动断层引起的地面位移之后指出,简单的滑动断层错动模式不能同时很好地解释观测到的邢台地震的水平和垂直形变。为了解释观测结果,提出了一个复合的断层模式。这个复合断层模式由六个简单的矩形滑动断层构成。运用网格尝试法,得到了基本上符合观测到的水平和垂直位移场的震源参数。结果是:第一、二、三部分,出露到地面,倾角45°,宽度15公里;第四、五、六部分,倾角82°,宽度30公里。其它参数是:断层面走向N35°E,倾向N125°E,断层总长度50公里,断层各部分的平均走向滑动错距依次为—78、—134、—17、2、—3和1厘米(负号表示右旋走向滑动,正号表示左旋走向滑动),平均倾向滑动错距依次为2、50、88、24、—5和—23厘米(负号表示逆断层,正号表示正断层),地震矩依次为3.2、5.9、3.7、2.0、0.5、1.9...

本文以完整的形式给出拉梅常数不相等情形的半无限弹性介质中任意倾角的矩形滑动断层引起的地震位移场解析表示式。以一些数值结果说明介质的泊松比、断层面的倾角、上界和下界对地面的地震位移场的影响。在比较1966年邢台地震的地形变资料和计算得到的各种走向、倾向、倾角、断层面长度、宽度、震源深度和错距的单个的矩形滑动断层引起的地面位移之后指出,简单的滑动断层错动模式不能同时很好地解释观测到的邢台地震的水平和垂直形变。为了解释观测结果,提出了一个复合的断层模式。这个复合断层模式由六个简单的矩形滑动断层构成。运用网格尝试法,得到了基本上符合观测到的水平和垂直位移场的震源参数。结果是:第一、二、三部分,出露到地面,倾角45°,宽度15公里;第四、五、六部分,倾角82°,宽度30公里。其它参数是:断层面走向N35°E,倾向N125°E,断层总长度50公里,断层各部分的平均走向滑动错距依次为—78、—134、—17、2、—3和1厘米(负号表示右旋走向滑动,正号表示左旋走向滑动),平均倾向滑动错距依次为2、50、88、24、—5和—23厘米(负号表示逆断层,正号表示正断层),地震矩依次为3.2、5.9、3.7、2.0、0.5、1.9×10~23达因·厘米,应力降依次为22、42、33、5、1、4巴,应变降依次为3.3、6.4、5.0、0.8

 
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