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philippine sea plate
相关语句
  菲律宾海板块
     The distribution of stresses is chiefly effected by philippine Sea Plate and Indian Ocean Plate.
     其应力分布主要受菲律宾海板块和印度洋板块的影响。
短句来源
     The movements occurred are related to the movements of Pacific plate, Philippine Sea plate and India-Australia plate rela- tive to Eurasia.
     这一系列运动的产生与南海周缘太平洋板块、菲律宾海板块和印度-澳大利亚板块在新生代期间与欧亚板块间的相对运动和相互作用有密切关系。
短句来源
     In the east the seismic slab of the Philippine Sea plate subducts at shallow dip angels between 10°~22° and its leading edge reaches down only to about 60~85km depth beneath Shikoku and the Kii peninsula.
     东部的菲律宾海板块地震俯冲带呈现出低角度俯冲 (10°~ 2 2°) ,且俯冲深度相当浅 (6 0~ 85km)的特征 ;
短句来源
     In the paper,we create an integral-rotation linear strain model for the Philippine Sea Plate(PHIL) on the basis of the ITRF2000 velocities of 7 sites on the PHIL.
     用菲律宾海板块上7个站ITRF2000的速度建立了菲律宾海板块的整体旋转线性应变模型.
短句来源
     The movement resulted from collision between the Philippine Sea plate and Eurasian plate in the Mindoro Island during 13 MaBP, and from collision between the Australian plate and the Eurasian plate in the Sulawesi Island during 10 MaBP.
     根据南海区域构造分析,产生这次构造运动的起因可能与菲律宾海板块和欧亚板块于13MaBP在民都洛岛处发生碰撞,以及澳大利亚板块和欧亚板块在苏拉威西岛处发生碰撞(10MaBP)有关。
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  “philippine sea plate”译为未确定词的双语例句
     APPLICATION AND COMPARISON OF TWO KINDS OF GPS INVERSE METHODS ON BORDER LAND BETWEEN PHILIPPINE SEA PLATE AND SOUTHWEST JAPAN
     两种GPS反演方法在日本西南与菲律宾板块交界处的应用与比较
短句来源
     (5) The subduction of Philippine Sea Plate and collision between Luson Arc and Taiwan made deep mark on volcanism in the Okinawa Trough.
     (5)海槽火山活动明显受菲律宾板块俯冲方向及吕宋-台湾碰撞作用的影响。
短句来源
     Since the middle Miocene,the South China Sea had subducted beneath the Philippine Sea Plate along the Manila Trench,and the subduction prism came into being.
     自中中新世以来,南海洋壳开始沿着马尼拉海沟向菲律宾海微板块俯冲,形成增生楔中洋内俯冲增生部分;
短句来源
     These NNE and NE faults become a long transform fault system and formed a boundary between the eastern margin of China Continental Plate and Philippine Sea Plate.
     这些北北东向和北东向断层形成一条巨长的转换断层系列,也是中国大陆板块东缘与菲律宾洋块的一条边界。
短句来源
     The Philippine Sea Plate also moved northwestward and collided obliquely with the Asian continent since 6.5Ma B.P. . The arc-continent collision made the collision prism west of the subduction prism,together forming the Taiwan accretionary prism.
     与此同时菲律宾海微板块开始向NW方向移动,前缘的吕宋岛弧自6.5Ma B.P以来与亚洲陆缘斜向碰撞,形成增生楔中弧陆碰撞增生部分。
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  相似匹配句对
     PHILIPPINE SEA
     美国航空母舰之四十四 CV-47“菲律宾海”号
短句来源
     TERRAIN FEATURES OF THE PHILIPPINE SEA
     菲律宾海的地势特征
短句来源
     Airlifting From Philippine
     空运自Philippine
短句来源
     Blue is the Sea
     海蓝蓝
短句来源
     THE SKY AND THE SEA
     天空和海
短句来源
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  philippine sea plate
Taking into account the magma aging effect, we cannot explain the high 3He/4He ratios of the volcanic arc region by the slab melting of the subducting Philippine Sea plate.
      
- Along the Nankai trough in southwest Japan, due to the subduction of the Philippine Sea plate, great earthquakes have occurred repeatedly.
      
Horizontal as well as vertical displacement rate demonstrate significant interaction between the landward Kanto block and the Philippine Sea plate.
      
-A significant seasonality is found in the occurrence time of past great earthquakes (M≥ 7.9) in the northwestern margin of the Philippine Sea plate.
      
Seasonality of Great Earthquake Occurrence at the Northwestern Margin of the Philippine Sea Plate
      
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Taiwan Island situated between the Eurasia and Pacific plates can be supposed as a part of Western Pacific seismic belt. On the basis of the characteristics of geological tectonics, gravity anomaly, crustal structure and seismicity, Taiwan Island and adjucent regions may be divided into three seismotectonic zones, they are: I) Seismote-ctonic zone of eastern Taiwan. There earthquakes occurred along the western margin of Philippino Sea basin and in the volcanic arc, longitudinal valley and foreland...

Taiwan Island situated between the Eurasia and Pacific plates can be supposed as a part of Western Pacific seismic belt. On the basis of the characteristics of geological tectonics, gravity anomaly, crustal structure and seismicity, Taiwan Island and adjucent regions may be divided into three seismotectonic zones, they are: I) Seismote-ctonic zone of eastern Taiwan. There earthquakes occurred along the western margin of Philippino Sea basin and in the volcanic arc, longitudinal valley and foreland depre-sisson in Lan Yu and Huo Shao Dao Islet. It is characterized by strong seismicity, high frequency of earthquake, NNE running distribution of epicenters and the NW-NWW running orientation of regional principal compressive stress field; 2) Seismotectonic zone of western Taiwan. There earthquakes appeared along the Cenozoic folding belt of Taiwan and marginal depression. Both seismicity and seismic frequency in this zone are much less than that of the eastern zone. Here the epicenters are distributed along NNE direction and the predominant principal compressive stress runs in NW-near EW direction, and 3) Seismotectonic zone of northern Taiwan. There earthquakes took place along the intersection zone of Taiwan and Ryukyu arcuated system with strong magnitude (intensity) and high frequency. The predominant principal compressive stress disclosed by the focal mechanism appears to be the direction approximately SN-NNW.In general, seismicities in Taiwan Island and the adjacent regions are varying with the relative motion between the Chinese and the Philippine Sea plates. In accordance with the view of plate tectonics, there are two types of earthquakes occurred in the region, that are. interplate earthquakes and marginal earthquakes of intraplate (namely arcuated island type of earthquakes), influenced by the boundary motion of plates. From the interplate earthquakes may be also recognized trench type and collisional type of earthquakes. The former was distributed in seismotectonic zone of northern Taiwan; and the NW running faults revealed by the focal mechanism are mostly of thrust faults, occationally of normal faults. The mechanism of thrust faults probably reveals the earthquakes caused by underthrusting action of plates along the trench, while the mechanism of normal faults seems to be used to illustrate the earthquakes caused by exten-sional faulting of lithosphere beneath the Philippine Sea plate. The collision type of earthquakes, as a result of strike-slip thrusting between the Chinese and the Philippine Sea plates, are mainly distributed in seismotectonic zone of eastern Taiwan. As to the island arc. type of earthquakes, they were distributed in seismotectonic zone of western Taiwan resulting from NNE running strike-slip thrusting within earth's crust.

本文在简要地论述了台湾岛及其周围地区的地质构造、重力异常、地壳结构和地震活动等特征的基础上划分了地震构造带,对台湾岛上7级以上强震的发震构造条件作了初步讨论,最后用板块构造观点探讨了本区地震的构造成因。

A calculation of present .tectonic stress field of China and its vicinity as a plane stress problem has been made by means of the finite element method. The crust of this region is taken as an elastic plate which composed of 12 parts with different Young's modulus E, Poisson's ratio v and thickness T. The whole region is divided into 288 trianglar elements. Five models of boundary conditions of stress and displace-ment have been considered, which represent relative values of the stress applied to the region...

A calculation of present .tectonic stress field of China and its vicinity as a plane stress problem has been made by means of the finite element method. The crust of this region is taken as an elastic plate which composed of 12 parts with different Young's modulus E, Poisson's ratio v and thickness T. The whole region is divided into 288 trianglar elements. Five models of boundary conditions of stress and displace-ment have been considered, which represent relative values of the stress applied to the region inside China and its vicinity by the Indian ocean plate, the Pacific plate and the Philippine sea plate respectively. The values of maximum shear stress obtained from calculation have been compared with the distribution of the strong earthquakes, and the directions of the maximum compressive principal stress with that obtained from focal mechanism solutions. The boundary condition which agrees most satisfac-torily with the actual has been selected as an available model. The result shows that the driving force seems to be mainly due to the Indian ocean plate. It is about two times larger than that of the Pacific plate and the Philippine sea plate respectively.

我国及邻区的现代构造应力场作为一平面应力问题用有限单元法进行了计算。将本区地壳看成是一不均匀的弹性板,根据各地区杨氏模量E、泊松比v和地壳厚度T的不同,组成12种材料区。全区被分成288个三角形单元。考虑了五种应力和位移边界条件,这些边界条件分别反映了印度洋板块、太平洋板块及菲律宾海板块对我国及邻区施加应力的相对大小。将计算得到的最大剪应力值与强震分布进行对比,将最大主压应力方向与震源机制解的最大主压应力方向进行对比,选择一种和实际符合得最好的边界条件作为可取的模式。结果表明:来自印度洋板块的作用力最大,大约是来自太平洋板块和菲律宾海板块作用力的两倍。

The forth paper briefly discusses earthquakes along continental margins,suggesting that the earthquake activities along the continental margins of eastern China can be divided into two seismic belts,namely the Taiwan-Ryukyu plate marginal seismic belt and the continental intraplate seismic belt,both are seperately controlled by motion of the Philippine Sea plate and block-faulted tectonics within the Eurasian plate.

介绍了大陆边缘地震的研究概况,主要分析了中国东部的陆缘地震可分为台湾——琉球板缘地震带和大陆架板内地震带。这两个地震带分别受到菲律宾海板块运动以及欧亚板块内部断块构造的控制。

 
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