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首页> 外文期刊>Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth >Indentation of the Philippine Sea plate by the Eurasia plate in Taiwan: Details from recent marine seismological experiments
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Indentation of the Philippine Sea plate by the Eurasia plate in Taiwan: Details from recent marine seismological experiments

机译:台湾欧亚大陆板块对菲律宾海板块的压痕:最新海洋地震实验的详细信息

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摘要

We analyze in this study a new set of marine data including 3D local tomography, 1992-2008 relocated earthquakes and two recent multichannel seismic lines to characterize the deformation style in the collision area offshore east Taiwan. We have mapped in detail the Mohos of the converging plates as well as the subduction interface with a resolution never reached before. We show that the sharp continental subduction of the Eurasia plate, beneath the middle part of the Central Range, indents the Philippine Sea plate (PSP) as attested by intra-oceanic slicing and incipient subduction of the PSP beneath the east coast of Taiwan. The westernmost part of the PSP slab is probably experiencing a beginning of break-off as attested by NW-trending en-échelon shear zones beneath the southern slope of the southern Ryukyu arc (SRA). These en-échelon shear zones have a sinistral component favored by the "collision-free" subduction of the PSP north of 24°30'N. The down-faulting of the subduction interface forms ramps along which earthquakes clusterize. Three M7 subduction earthquakes occurred offshore Suao city along these ramps with a recurrence interval of about 40years: 1920 M_w7.7, 1963 M_w7.2 and 2002 M_w7.1 events. The 1966 M_w6.0-7.5 earthquakes sequence likely outlines a WNW-ESE left-lateral intra-slab shear zone. The SRA upper plate accommodates the complex geometry and deformation of the subducting PSP through seismic deformation. Shallow high velocities fringing the Luzon volcanic arc (LVA) beneath the Longitudinal Valley and north of the southernmost Ryukyu forearc basins are interpreted as relics of the LVA forearc basement squeezed in the collision zone. Based on the accommodation of a large part of the convergence through shortening within the PSP and the subsequent segmentation of the shallow subduction interface, we consider that the nucleation of a M_w≥8 earthquake along the southernmost Ryukyu megathrust is unlikely.
机译:在这项研究中,我们分析了一组新的海洋数据,包括3D局部层析成像,1992-2008年重新定位的地震以及两条最近的多通道地震线,以表征台湾东部近海碰撞区的变形方式。我们详细绘制了会聚板的Mohos以及俯冲界面的分辨率,这是以前从未达到过的。我们显示,中部山脉中部以下的欧亚大陆板块急剧的大陆俯冲,缩进了菲律宾海板块(PSP),这是由台湾东海岸以下的海内切片和PSP的初期俯冲所证实的。 PSP平板的最西端可能正在经历断裂的开始,这是由琉球南弧(SRA)南部斜坡下方的西北走向的大阶梯剪切带证实的。这些梯级剪切带的正弦分量受北太平洋24°30'N处PSP的“无碰撞”俯冲的影响。俯冲界面的断层形成了斜坡,地震沿这些斜坡聚集。苏澳市近海沿这些坡道发生了3次M7俯冲地震,重复间隔约40年:1920 M_w7.7、1963 M_w7.2和2002 M_w7.1事件。 1966年的M_w6.0-7.5地震序列很可能勾勒出WNW-ESE板坯左外侧剪切带。 SRA上板通过地震变形来适应俯冲PSP的复杂几何形状和变形。在纵谷下方和最南端的琉球前陆盆地以北的吕宋火山弧(LVA)边缘的浅层高速被解释为在碰撞带中挤压的左伏前臂基底的遗迹。基于通过PSP内的缩短和随后的浅层俯冲界面的分割来适应大部分收敛,我们认为沿着最南端的琉球巨推力发生M_w≥8地震成核的可能性很小。

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