首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >A three-dimensional seismic wave speed model in southwestern Japan from combined use of waveform modeling and travel-time tomography
【24h】

A three-dimensional seismic wave speed model in southwestern Japan from combined use of waveform modeling and travel-time tomography

机译:结合波形建模和行进时间层析成像技术在日本西南部建立的三维地震波速度模型

获取原文
获取原文并翻译 | 示例
       

摘要

Recent three-dimensional (3-D) travel-time tomographic models of southwestern (SW) Japan image the subducting Philippine Sea plate (PHSP) and low velocity anomalies with long-wavelength spatial resolution. However, the agreement between the synthetics calculated with the existing 3-D model and data is not satisfactory for sP and S waves in the higher frequency range (0.2Hz). The unsatisfactory agreement can be attributed to the parameters of the initial wave speed model for the tomographic inversion, as well as the difficulty in detecting S-wave travel times accurately. In order to improve the wave speed model, we first constructed a 3-D reference model by forward modeling using waveform data from an intraslab earthquake and then performed repeated travel-time inversions using the 3-D reference model as the initial model. The newly derived high-resolution model 3DM-SWJ can produce synthetics that are substantially in better agreement with the data than previous models. The distribution of high P-wave to S-wave speed ratios (V _P/V _S) calculated from model 3DM-SWJ shows short-wavelength heterogeneities that could have been formed in relation to the subduction of the Philippine Sea Plate beneath the Eurasian plate. This combined use of forward waveform modeling for slab and crust configuration and repeated tomographic inversion of travel-times provides a better 3-D structural model of seismic properties for understanding tectonic features related to the subduction process, in addition to better estimating ground motions.
机译:日本西南(SW)最近的三维(3-D)行进时层析成像模型对菲律宾俯冲的菲律宾海板(PHSP)和低速异常具有长波长空间分辨率进行了成像。但是,对于较高频率范围(0.2Hz)中的sP和S波,使用现有3-D模型计算的合成信号与数据之间的一致性并不令人满意。不能令人满意的协议可以归因于用于层析X射线反演的初始波速模型的参数,以及难以准确检测S波传播时间的原因。为了改善波速模型,我们首先使用板内地震的波形数据通过正向建模来构建3-D参考模型,然后使用3-D参考模型作为初始模型进行重复的传播时间反演。新推导的高分辨率模型3DM-SWJ可以生成比以前的模型与数据更好地吻合的合成模型。由3DM-SWJ模型计算得出的高P波与S波速比(V _P / V _S)的分布表明,短波非均质性可能与欧亚板块下方菲律宾海板块的俯冲有关。平板和地壳构造的正向波形建模以及行进时间的断层层析反演的这种结合使用,除了可以更好地估计地震动外,还提供了更好的地震属性3-D结构模型,以了解与俯冲过程有关的构造特征。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号