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An elastic plate model for interseismic deformation in subduction zones

机译:俯冲带间震变形的弹性板模型

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Geodetic observations of interseismic surface deformation in the vicinity ofsubduction zones are frequently interpreted using simple kinematic elastic dislocationmodels (EDM). In this theoretical study, we develop a kinematic EDM that simulates platesubduction over the interseismic period (the elastic subducting plate model (ESPM))having only 2 more degrees of freedom than the well-established back slip model (BSM):an elastic plate thickness and the fraction of flexural stresses due to bending at the trenchthat are released continuously. Unlike the BSM, in which steady state deformation in bothplates is assumed to be negligible, the ESPM includes deformation in the subductingand overriding plates (owing to plate thickness), while still preserving the correct sense ofconvergence velocity between the subducting and overriding plates, as well as zero netsteady state vertical offset between the two plates when integrated over many seismiccycles. The ESPM links elastic plate flexure processes to interseismic deformation andhelps clarify under what conditions the BSM is appropriate for fitting interseismicgeodetic data at convergent margins. We show that the ESPM is identical to the BSM inthe limiting case of zero plate thickness, thereby providing an alternative motivation forthe BSM. The ESPM also provides a consistent convention for applying the BSM to anymegathrust interface geometry. Even in the case of nonnegligible plate thickness, thedeformation field predicted by the ESPM reduces to that of the BSM if stresses related toplate flexure at the trench are released either continuously and completely at shallowdepths during the interseismic period or deep in the subduction zone (below 100 km).However, if at least a portion of these stresses are not continuously released in the shallowportion of the subduction zone (via seismic or aseismic events), then the predicted surfacevelocities of these two models can differ significantly at horizontal distances from thetrench equivalent to a few times the effective interseismic locking depth.
机译:俯冲带附近地震表面形变的大地观测经常使用简单的运动弹性位错模型(EDM)来解释。在此理论研究中,我们开发了一种运动EDM,该运动EDM在地震期间模拟板俯冲(弹性俯冲板模型(ESPM))仅比公认的后滑动模型(BSM)多2个自由度:弹性板厚度以及由于沟槽弯曲而引起的弯曲应力的分数不断释放。与BSM不同,在BSM中假定两个板块的稳态变形都可以忽略不计,ESPM包括俯冲板块和上覆板块的变形(由于板厚),同时仍保留了俯冲板块和上覆板块之间的正确收敛速度感。当在许多地震周期中积分时,两个板块之间的垂直净零位移为零。 ESPM将弹性板的挠曲过程与地震之间的变形联系起来,并有助于阐明在什么条件下BSM适合在收敛边缘处拟合地震大地数据。我们证明,在零板厚的极限情况下,ESPM与BSM相同,从而为BSM提供了替代动机。 ESPM还提供了将BSM应用于任何大型推力接口几何形状的一致约定。即使在板厚度不可忽略的情况下,如果与沟槽弯曲有关的应力在地震期间的浅深度连续或完全释放,或者在俯冲带的深处(小于100),则由ESPM预测的变形场也会减小到BSM的变形场。但是,如果至少一部分应力没有在俯冲带的浅部分中连续释放(通过地震或地震事件),则这两个模型的预测表面速度在距海沟的水平距离等于有效隔震锁定深度的几倍。

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