板块运动,plate movement
1)plate movement板块运动
1.So the authors consider that the formation and evolution of the Chinese inland basins are the necessary result ofplate movements since Paleozoic.盆地的形成和演化与板块运动有密不可分的关系 ,可以说中国陆相盆地的形成和演化是古生代以来板块运动的必然产物。
2.For this information, it can be induced that the rotative velocity of the liguid outer core presents similar nonuniformity, and the nonuniform rotation will have an effect on crustplate movement.据此,作者推测液态外地核的自转,也存在类似的不均匀性,而这种不均匀自转将对地壳板块运动产生影响。
3.In order to surmount many deficiencies in determining the parameters ofplate movement by least square(LS) method,we have set up a semiparametric model based on compensated LS principle.为避免最小二乘法求解板块运动参数的诸多不足,建立了基于补偿最小二乘原理的半参数板块运动模型,并利用最新的ITRF速度场求解出全球各主要板块运动的欧拉矢量。
英文短句/例句
1.The movement of plates is dangerous.板块运动是非常危险的。
2.Variable Viscosity Whole Mantle Convection and Surface Plate Motions;全球变粘度地幔对流与地表板块运动
3.ON MAN CI;论奇偶言板块运动的高速状态──慢词
4.Establishing of Background Field of Global Plate Motion and ITRFVEL全球板块运动背景场及ITRFVEL的建立
5.Global Plate Motion Model Based on ITRF基于ITRF的全球板块运动模型
6.Geologists describe the motion of the plates and the consequences of such motion as plate tectonics.地质学家把板块运动及这种运动所造成的后果看作是板块构造运动。
7.ON SPHERICAL MANTLE MIXTURE DRIVEN BY MODERN PLATE TECTONIC MOTION现代板块运动驱动球域地幔混合的研究
8.Analysing the Extending of Atlantic Based on Global Plate Motion Models基于全球板块运动模型分析大西洋扩张变化
9.Global Plate Motion and its Impact on the Earth′s Surface Area Changes全球板块运动及其对地球表面积变化的影响
10.The movement of the plates strains the rock at and near plate boundaries and produces zones of faults around these boundaries.板块运动在板块边界或者附近拉张岩石，并且在边界周围产生断层带。
11.If this were not the case, the Earth would be covered by a single spherical plate, and no relative plate motion could occur.如果不是这种情况，地球就会被一个单独的球状板块所覆盖，并且不会有相对的板块运动发生。
12.The most commonly cited mechanism for transforming thermal energy into the movement of plates is the action of plumes.将热能转换成板块运动最普遍被引用的机制，是地幔羽的活动。
13.In this point, when the deadlock ends and motion of the two plates resumes, an earthquake will occur.”在这时，随着剧烈挤压的结束和两个板块运动的恢复，就会发生地震。
14.Plate Tectonics and Geodynamics of Orogenesis of the Southwest Tianshan Mountains;西南天山板块构造及造山运动动力学
15.Mountain Building occurs during rapid subduction of one plate under another.当一个板块迅速地挤压到另一个板块下面时会发生造山运动。
16.INTERACTION BETWEEN PHILIPPINE SEA PLATE (PH) AND EURASIA (EU) PLATE AND ITS INFLUENCE ON THE MOVEMENT EASTERN ASIA菲律宾海板块与欧亚板块的相互作用及其对东亚构造运动的影响
17.The Clinical Significance of Combining Treadmill Exercise Test (TET) with Carotid Artery Plaque Inspection in Diagnosis of Coronary Heart Disease;平板运动试验结合颈动脉斑块检测诊断冠心病
18.Separate rock layers, or plates, under the oceans and continents move very slowly.海洋和陆地下面的岩石层或板块在缓慢地运动。
相关短句/例句
plate motion板块运动
1.This paper gives a background review of geodynamical researches onplate motion,introduces the internal wave hypothesis and latitudinal normal density hypothesis presented by Chinese scholars recently.本文简要介绍了大陆漂移及板块运动动力问题研究的历史背景、以及我国地学工作者最新提出的“内波假说”和“纬向正常密度假说”在这一问题上的基本观点。
2.Under the deformation analysis model composed of rigidplate motion + uniform strain of the plate + inner non-homogeneous strain of the plate, the movement and deformation of each main plate of the globe have been studied based on the velocity field data announced by IERS in the frame of ITRF2000 at 657 GPS,SLR and VLBI stations distributed on main plates.利用IERS所公布的分在全球各大构造板块上的 6 5 7个GPS、SLR和VLBI连续观测站在ITRF框架下的速度场资料 ,采用刚体板块运动 +板块整体均匀应变 +板块内局部不均匀应变的变形分析模型 ,研究了全球各主要板块的运动和变形。
3.In this paper, a new present-day globalplate motion ITRF2000VEL is determined on the basis of space geodetic data, incorporating the ITRF2000 velocity fi.基于现代空间测量技术 SL R、VL BI和 GPS实测资料 ,解算出大西洋中脊海底扩张速率 ,其中北大西洋的东西向扩张速率平均为 35 mm/ a,赤道大西洋东西向扩张速率分别为 2 0～ 2 5 mm/ a,南大西洋东西向扩张速率为 2 2～2 8mm/ a,证实全球板块运动的存在及大西洋扩张学说 ,并基于全球几百万年地质模型 NNR- NU VEL1A,北大西洋的东西向扩张速率平均为 2 4。
3)movement of plate or block mass板(地)块运动
4)plate kinetics板块运动学
5)plate motion model板块运动模型
1.This paper derives aplate motion model called GVM1 based on space geodesy techniques by the integrated data of GPS and VLBI.利用GPS和VLBI的组合数据,解算了北美、欧亚、太平洋等12板块之间的相对运动欧拉矢量,得到了实测的板块运动模型GVM1。
2.Then,we established the new globalplate motion model—— ITRFVEL.简要分析了最新的国际地球参考框架ITRF实现的基本情况及其相对于ITRF2000的改进,以ITRF为参考框架建立了新的全球板块运动模型ITRFVEL。
6)instantaneous plate motion现时板块运动
1.We get more steadyinstantaneous plate motion parameters by analyzing and refining the station velocity residuals.采用截止到GPS观测数据和1997年的VLBI观测数据,利用它们的站速度信息,组合解算完全基于空间技术的板块运动参数;通过对站速度残差的精化分析,得出更加稳健的现时板块运动参数;并通过反复试算得出稳定台站的选取以及台站的分布对板块运动欧拉极有很大的影响。
延伸阅读
南美洲运动会和南十字运动会19在巴西举行过1届南美洲运动会,参加者限于南美洲国家。1978年在玻利维亚举行过 1届南十字运动会，参加国有阿根廷、玻利维亚、巴西、智利、厄瓜多尔、巴拉圭、秘鲁和乌拉圭8国。
