菲律宾海板块

菲律宾海板块的整体旋转线性应变模型与板内形变-应变场

Integral-rotation linear strain model and intraplate deformation-strain field of the Philippine Sea Plate

其应力分布主要受菲律宾海板块和印度洋板块的影响。

The distribution of stresses is chiefly effected by philippine Sea Plate and Indian Ocean Plate .

结果表明，本区既受到来自太平洋－菲律宾海板块向NW方向的挤压作用，又受到来自印度板块向N向E的挤压。

The result shows that the extruding has been subject to both the Pacific-Philippines Sea Plate in the NW direction and the Indo Plate in the N and E directions .

本文模型与Sella等建立的刚体运动模型相比能更精确地描述菲律宾海板块的现今构造运动与板内形变。

Compared with the rigid motion model created by Sella et al . , our model is capable to accurately describe the current-day tectonic movement and intraplate deformation of the PHIL .

讨论了西太平洋俯冲带的分布及特征、西太平洋Wadati－Benioff带的形态及俯冲带上的应力状态及太平洋板块、菲律宾海板块与欧亚板块之间的相互作用；

The distribution and characteristics of the subduction zone , configuration of the Wadati - Benioff zone and the stress state of the subduction zone in the western Pacific region were studied ;

观测资料显示，菲律宾海板块一直以西北方向向台湾陆地挤压；

The Philippines sea plate continuously compresses Taiwan northwestwards .

日本中部菲律宾海板块和欧亚板块之间的地震平静边界

The seismically quiescent boundary between the Philippine Sea plate and the Eurasian plate in central Japan

台湾西部和台湾海峡的地震活动也受到菲律宾海板块的控制。

Seismicity of the western Taiwan and the Taiwan Strait is also affected by the Philippine Sea Plate .

台湾纵谷断层是菲律宾海板块与欧亚板块之间碰撞挤压边界。

The Longitudinal Valley fault of Taiwan is the boundary of collision and compression between the Eurasian and Philippine Sea plates .

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

Interaction between Philippine Sea plate ( ph ) and Eurasia ( eu ) plate and its influence on the movement Eastern Asia

这种非同步发展可能是由于菲律宾海板块向亚洲大陆俯冲过程中，其速度在时间和空间上的差异性所致。

The developmental differences are caused by different subduction velocities in time and space of the Philippine Sea Plate toward the Asia Continent .

台湾地区是由于欧亚板块和菲律宾海板块相互作用而形成的特殊的俯冲带和碰撞带。

Taiwan orogen resulting from the interaction between the Eurasian and Philippine Sea ( PHS ) plates is a subduction and collision zone .

结果清晰地显示出呈高速异常体的菲律宾海板块和地幔楔中的低速异常体，这与前人的研究结果相符合。

Our tomography results show very clearly high-velocity anomalies corresponding to the subducting Philippine Sea slab and low-velocity anomalies in the mantle wedge .

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。

The movements occurred are related to the movements of Pacific plate , Philippine Sea plate and India-Australia plate rela - tive to Eurasia .

菲律宾海板块主应变场的空间变化与板块内部及周围的构造背景密切相关，是构造应力场的反映。

Closely related to the intraplate and surrounding tectonic settings , the spatial variation of the principal strain field of the PHIL is a reflection of the tectonic stress field .

赞岐岩的形成与菲律宾海板块年轻的热的岩石圈俯冲和四国盆地的张开有关，产于岛弧的弧前或弧后盆地环境。赞岐岩不只代表火山岩，也包括侵入岩。

The Setouchi sanukite is located in fore - or back-arc basins , and originated in subduction of the young and hot Philippine Sea plate and pull-apart of the Shikoku basin .

通过综合分析表明，本区大致承受北北西&南南东方向的挤压作用，即菲律宾海板块与欧亚板块碰撞挤压的结果。

By synthetic analysis of data concerned this region is determined to be compressed from NNW-SSE direction , due to the collision between the Phillippine Sea plate and the Eurasian plate .

台湾岛以南海域（台南滨海）弧陆碰撞带位于欧亚板块、菲律宾海板块和南海的结合部位，是新近纪弧陆碰撞研究的理想场所。

The offshore Taiwan arc-continent collisional orogen was situated in the conjunction area of the Eurasian plate , the Philippine Sea plate and the South China Sea , which was created in Neogene .

结果表明，作为欧亚大陆板块与太平洋菲律宾海板块的边界断裂之一的中央山脉断裂第四纪以来乃至现今仍具有强烈的活动，因而发生了4次M≥7地震；

The results show , as one of the boundary faults between the Eurasian Plate and the Pacific Philippine Ocean Plate , the Central Mountian Fault has acted strongly since Quaternary , so earthquakes with magnitude ≥ 7.0 occured 4 times ;

菲律宾海板块在台湾岛东部与欧亚板块的碰撞俯冲是台海地区地壳运动、变形和发生大地震的主要驱动力。

The collision and underthrust of Philippine Sea plate with Eurasian plate in the eastern part of Taiwan Island can be considered as the principal force for the crustal movement , deformation and great earthquake occurred in Taiwan and its coastal area .

来自北西向运动的菲律宾海板块构造应力控制了从台湾纵谷、华南块体，直到中国南北地震带南段东部地域的应力场。

The stress field due to the northwestward motion of the Philippine Sea plate controls the stress field of the lithosphere from the Longitudinal Valley of Taiwan through the South China block to the eastern part of the southern segment of the North-South Seismic Belt .

中新生代时期，欧亚板块、太平洋-菲律宾海板块、印度-澳大利亚板块等几大板块之间的相对运动和相互作用，导致南海中、南部形成复杂的断裂体系和构造格局。

The complicated fracture systems and tectonic framework were formed in the central and southern parts of the South China Sea due to the reciprocal movement of the plates like the Euro-Asia Plate , the Pacific-Philippine Plate and the India-Australia Plate during Mesozoic and Cenozoic .

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。

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 .

菲律宾海板块在台湾东海岸向北西西方向的挤压碰撞作用是台湾地区和闽粤赣交界地区强震孕育和发生的最直接最主要的动力来源。

The compression and collision to the east coast of Taiwan from Philippine block moving to the west-northwest is the most direct force cause of the strong earthquake to breeding and happening in Taiwan area and the border area among Fujian , Guangdong and Jiangxi Provinces .

总体结果表明，中国大陆及其周缘岩石圈应力场和构造运动可以归结为印度洋板块、太平洋板块、菲律宾海板块与欧亚板块之间相对运动，以及大陆板内区域块体之间的相互作用的结果。

The results suggest that the stress field of the lithosphere and tectonic movement in and around continental China are attributable to the motions of the Eurasian plate relative to the Indian , Pacific and Philippine Sea plates and interactions among blocks within the continental plate .

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；

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 .

台湾增生楔位于欧亚板块、菲律宾海微板块和南海的结合部位，是现代弧陆碰撞研究的理想场所。

Taiwan accretionary prism lies in the conjunction area of the Eurasian Plate , the Philippine Sea Plate and the South China Sea , and is characterized by the young age of the arc-continent collision .