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slip movement
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  滑运动
     Calculation indicates that the average rate of sinistral strike\|slip movement in the Holocene time amounts to 1.11±0.09~2.69±0 24 mm/a along the Huanggangshui fault and 3.26±0.26 mm/a along the Fengshun\|Shantou fault.
     经计算 ,黄岗水断裂和丰顺 -汕头断裂的全新世左旋走滑运动平均速率分别达 1 11±0 0 9~ 2 6 9± 0 2 4mm a和 3 2 6± 0 2 6mm a。
短句来源
     The result shows that whole differential movement is counterclockwise, with a principal compressive stress azimuth of 72°. There is no obvious strike slip movement along two sides of the fault.
     结果表明,整体呈现逆时针的差异活动,主压应力场的方位角为72°,断裂两侧不存在明显的走滑运动
短句来源
     (2) Gansu-Qinghai block in the south of this area moves faster, while Alashan block in the north of this area moves slower, the difference of the velocity between two blocks is near 6mm/a, the sinistral strike slip movement of Qilian-Haiyuan fracture zone is much more remarkable;
     ②南部的甘肃—青海块体的运动较快 ,而北部的阿拉善块体的运动较慢 ,二者运动速率相差近 6mm/a,祁连—海原断裂带左旋走滑运动显著 .
短句来源
     The first squeezing out stage that occurred during the middle and late Miocene(12~5?Ma)was remarkably characterized by tectonic deformations of strong left lateral strike slip movement of Xianshuihe fault zone,right lateral strike slip movement of Honghe fault,and east ward squeezing out of Chuan Dian(Sichuan Yunnan)block.
     研究结果表明 ,第一阶段构造挤出发生在中新世中晚期的 12~5Ma期间 ,最显著的构造形变特征是鲜水河断裂带强烈的左旋走滑运动、红河断裂右旋走滑运动和川滇地块向东挤出。
短句来源
     On the basis of an integrated study of the structural features of the boundary fault of the basin, migration of the depocenter of the basin and sedimentary characteristics of the turbidites of the Laiyang Group, the paper discusses the relation of the formation of the turbidites of the Laiyang Group with the strike slip movement of the Tanlu (Tancheng Lujiang) fault during the Early Cretaceous.
     在综合盆地边界断裂的构造形迹、盆地沉积中心的迁移状态以及浊积地层沉积特征的基础上,讨论了莱阳群浊积地层形成与郯庐断裂早白垩世走滑运动的关系。
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  滑活动
     The Main Gaoligong shear zone was formed under the metamorphic conditions equivalent to high greenshist to low amphibolite facies during the Neogene dextral strike slip movement.
     认为高黎贡剪切带是在相当于高绿片岩相—低角闪岩相的变质条件下形成的,是晚第三纪右旋走滑活动的产物。
短句来源
     The secular GPS crustal deformation image has reflected the relatively complete left lateral strike slip movement of this active fault zone.
     长趋势GPS地壳形变图像反映了这条活动断裂带相对完整的左旋走滑活动
短句来源
  “slip movement”译为未确定词的双语例句
     The Bohai Bay Basin was developed in a dextral transtensional tectonic setting during the Cenozoic, therefore, strike slip movement was one of major controlling factors on structural deformation,basin formation and hydrocarbon accumulation.
     渤海湾盆地形成于新生代右旋扭张构造背景 ,走滑作用是新生代构造变形、盆地形成和油气聚集的主要控制因素之一。
短句来源
     According to the features of the basining and tectonic evolution of the Nanchang subbasin,the authors suggest that the large-scale sinistral strike-slip movement of the Ganjiang fault zone occurred in the early-mid Late Cretaceous and the turning point from the sinistral strike slip movement to dextral strike-slip movement occurred at the end of the Late Cretaceous early Nanxiongian(K_2n1).
     据南昌凹陷的成盆演化特征推断赣江断裂带大规模左行走滑的时代为晚白垩世早、中期,转折点在南雄早期K2n1末。
短句来源
     By means of slip movement boundary condition, two decisive factors of particle group and wall friction are analyzed: friction factor and normal pressure, the expression for calculating friction is given and is used for simulating viscous flow model for descending of coke in CDQ chamber.
     采用滑移边界条件,分析了颗粒群与壁面摩擦力的2个决定因素:摩擦系数和法向压力,提出了摩擦力计算表达式,并应用于模拟干熄炉内焦炭运动的粘性流模型。
短句来源
     SURFACE CHARACTERISTICS OF QUATERNARY ACTIVITY AND GEOLOGICAL EVIDENCES OF STICK SLIP MOVEMENT OF KEKETUO OCEAN-ERTAI FAULT
     可可托海—二台断层第四纪活动的地表特征和粘滑运动的地质证据
短句来源
     The NNE striking Tanlu fault zone bounds the extensional domains on the east and displays right lateral strike slip movement, consistent with EW trending compression and N S trending extension.
     N N E走向的郯庐断裂带构成了华北引张构造域的东界,表现为右旋走滑,与 E W 向挤压和 S N 向引张构造应力作用一致。
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  slip movement
The gouges showed nearly identical strength behaviors at the two sliding velocities; all four gouges, however, showed a greater tendency to stick-slip movement and somewhat higher stress drops in the experiments at 4.8×10-2 μm/sec.
      
The lateral (frictional) force map shows all characteristics of the stick-slip movement of the probing tip.
      
The orientation of the principal stresses confirms the sinistral strike-slip movement along the Novy Kostel-Po?átky-Zwota line (the trend is about 355°) defined by the epicentres of the micro-earthquakes.
      
Four events located at an offset of the rise near 41.5° N may be related to strike-slip movement on a developing transform fault.
      
Morphology and sediments suggest that the principal locus of strike-slip movement within the fracture zone probably migrated incrementally westward from one fault-trough to another.
      
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Fault plane solutions are obtained from data of the first motions for 24 earthquakes with Ms ≥ 4.0 of the Haicheng earthquake sequence, the mainshock of which occurred on Feb. 4, 1975. One of the nodal planes of the mainshock strikes N 70° W, dipping 80° to the NE. while the other nodal plane strikes N 23° B, dipping 75° to the SE. Based on the data of the spatial distributions of the after shocks and the ground deformations, the N 70° W nodal plane is taken as the fault plane. The faulting is nearly a vertical,...

Fault plane solutions are obtained from data of the first motions for 24 earthquakes with Ms ≥ 4.0 of the Haicheng earthquake sequence, the mainshock of which occurred on Feb. 4, 1975. One of the nodal planes of the mainshock strikes N 70° W, dipping 80° to the NE. while the other nodal plane strikes N 23° B, dipping 75° to the SE. Based on the data of the spatial distributions of the after shocks and the ground deformations, the N 70° W nodal plane is taken as the fault plane. The faulting is nearly a vertical, left-lateral strike-slip with a minor component of normal dip-slip movement. While the focal mechanisms of all the fore-shocks and most of the aftershocks are similar to that of the mainshock, those of 4 aftershocks with Ms ≥ 4.0 are remarkably different from the mainshock. They represent a faulting with slip vector reversed in direction to that of the mainshock. One possible explanation for these exceptions is that during the mainshock the fault movement overshot along some segments of the fault.The source parameters of the mainshock are calculated from the data of field observations and spatial distributions of the aftershocks. The fault length, width, averge dislocation, seismic moment, and stress-drop, of the mainshock, are estimated as 70 km, 20km, 45cm, 2.1 x 1026 dyne·cm, 4.8 bars, respectively. It is a low stress-drop earthquake occurring in a weak zone that is incapable of accumulating higher stresses.For 81 foreshocks and aftershocks the source dimensions, seismic moments, stress-drops as well as average dislocations are calculated from the data of the first half cycles and amplitudes of the seismic P-waves. The results indicate that the stress-drops are rather low, and generally in the range of 0.1-1.0 bars, for both the foreshocks and aftershocks. There are two regions with relatively higher stress-drops ( ≥ 0.8 bars), which correspond to the overshooting portions on the main fracture. These results imply that there might be some intrinsic connections between higher initial stresses before the mainshock, overshooting of fault movment, relatively higher stress-drops, and reverse of the slip vectors of focal mechanisms. It seems that the latter three phenomena are the results of the relatively higher initial stress.

由地震纵波初动符号的资料,求得了海城地震系列中Ms≥4.0的24个地震的断层面解。主震发生于1975年2月4日,它的一个节面走向N70°W,倾向NE,倾角81°;另一个节面走向N23°E,倾向SE,倾角75°。根据余震的空间分布以及地面形变资料选取N70°W的节面为断层面,主震是发生在这个近乎直立的断层面上的左旋走向滑动,略具正的倾向滑动分量。前震及大多数余震的震源机制和主震的相似,有四个Ms≥4.0的余震的震源机制和主震的迥然不同,表现出滑动向量和主震的滑动向量相反的断层错动方式。这种情况的一种可能的解释是主震时在断层的一些地段发生错动过头。 由野外资料及余震的空间分布资料计算了主震的震源参数。主震断层长70公里,宽20公里,平均错距45厘米,地震矩2.1×10~(26)达因·厘米,应力降4.8巴,应变降7.3×10~(-6)。它是发生在不能积累起较高应力的薄弱地带的一次低应力降的地震。 由地震纵波初动的半周期和振幅的资料计算了81个前震和余震的震源尺度、地震矩、应力降和平均错距。结果表明前震和余震的应力降都比较低,一般在0.1—1巴之间。余震区中有两个应力降相对说来比较高(高于0.8巴)的地区,它们恰好对...

由地震纵波初动符号的资料,求得了海城地震系列中Ms≥4.0的24个地震的断层面解。主震发生于1975年2月4日,它的一个节面走向N70°W,倾向NE,倾角81°;另一个节面走向N23°E,倾向SE,倾角75°。根据余震的空间分布以及地面形变资料选取N70°W的节面为断层面,主震是发生在这个近乎直立的断层面上的左旋走向滑动,略具正的倾向滑动分量。前震及大多数余震的震源机制和主震的相似,有四个Ms≥4.0的余震的震源机制和主震的迥然不同,表现出滑动向量和主震的滑动向量相反的断层错动方式。这种情况的一种可能的解释是主震时在断层的一些地段发生错动过头。 由野外资料及余震的空间分布资料计算了主震的震源参数。主震断层长70公里,宽20公里,平均错距45厘米,地震矩2.1×10~(26)达因·厘米,应力降4.8巴,应变降7.3×10~(-6)。它是发生在不能积累起较高应力的薄弱地带的一次低应力降的地震。 由地震纵波初动的半周期和振幅的资料计算了81个前震和余震的震源尺度、地震矩、应力降和平均错距。结果表明前震和余震的应力降都比较低,一般在0.1—1巴之间。余震区中有两个应力降相对说来比较高(高于0.8巴)的地区,它们恰好对应于主破裂错动过头的部位。这些结果意味着震前高应力、错动过头、相对高应力降和震源机制反向四者之间?

On November 7, 1976, a strike slip fault type earthquake of magnitude 6.7 occurred in the border region of the two southwestern provinces, Sichuan and Yunnan, at the localities Ninglang and Yanyuan, About one year before the earthquake, the authors made a medium term prediction for the magnitude and epicenter of an impending strong earthquake, based on the result of analysis of the variation of seismic wave velocity ratio of a region of about 20,000 km2 in extent. The prediction is considered as more or...

On November 7, 1976, a strike slip fault type earthquake of magnitude 6.7 occurred in the border region of the two southwestern provinces, Sichuan and Yunnan, at the localities Ninglang and Yanyuan, About one year before the earthquake, the authors made a medium term prediction for the magnitude and epicenter of an impending strong earthquake, based on the result of analysis of the variation of seismic wave velocity ratio of a region of about 20,000 km2 in extent. The prediction is considered as more or less satisfactong. Of course, the imminent prediction of the time of occurrence was based on other precursory phenomena observed in the region.The results given in this article, may be taken as a new example, for the appearance of variation of velocity ratio before a strike-slip fault type earthquake. A preliminary discussion has been made on the results in consideration of the difference between shear fracturing and strike-slip movements as well as the anisotropy caused by dilatancy.

1976年11月7日,我国川滇两省交界处的盐源、宁蒗一带发生6.7级走滑断层型地震.震前约一年,作者根据附近约二万平方公里范围内的波速比普查结果,对未来主震的震级和地点作了比较符合实际的中期预报.发震时间的预报是后来根据其它前兆观测结果的综合分析作出的.本文可以作为走滑断层型地震前观测到波速比变化的一个新的实例.根据剪切破裂和粘滑运动之间的差别以及膨胀造成的各向异性,对有关结果作了初步讨论.

The anti xi-type seismic zones can be found along the Xianshuihe fault as the form of ground fractures, most of them in the form of alternative tensile-shear cracks with the compressional drumlins or the thrust. And the drumlins may usually appear in the gaps where the cracks run en echelion.On the basis of the field observations of the Daofu (M = 6.9) earthquake of 1981 and the information of the Luhuo (M = 7.9) earthquake of 1973, this paper discussed the mechanism of formation of the ground crack zones in...

The anti xi-type seismic zones can be found along the Xianshuihe fault as the form of ground fractures, most of them in the form of alternative tensile-shear cracks with the compressional drumlins or the thrust. And the drumlins may usually appear in the gaps where the cracks run en echelion.On the basis of the field observations of the Daofu (M = 6.9) earthquake of 1981 and the information of the Luhuo (M = 7.9) earthquake of 1973, this paper discussed the mechanism of formation of the ground crack zones in terms of photoelastic experiment on clay.The author inclined to consider the studied ground crack zones to be the result of strik-slip movement along the Xianshuihe fault and the drumlins in the gaps between en echelon cracks were generated due to resulting adjustment in the normal direction at both terminals of the cracks from their lateral displacement. According to the shape of the drumlins and thrusting direction the author came to a preliminary conclusion that this kind of ground crack zones can be accounted for by the SSE-trending movement of the Sichuan Yunnan rhombic fault block.

本文以1981年道孚6.9级地震考察资料为基础,结合1973年炉霍地震资料并运用光弹,泥料实验,讨论了鲜水河断裂上反“多”字型地裂缝带的成因机制。笔者认为反“多”字型地裂缝是断层水平剪切运动的产物,出现与相邻两条羽列裂缝交替部位的鼓包是裂缝水平错动在垂直方向调整作用的结果。鼓包两翼往往东陡西缓,鼓包轴部的逆断层也往往由西向东逆掩,这可能与断裂南西侧向南东运动有关,是以滇菱形断块向南南东运动产生的结果。

 
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