Mantle Dynamics of the Izu-Bonin Subduction System

本研究通过地震观测和数值模拟实验相结合，为伊豆-波宁俯冲系统的地幔流动和动力学提供了新的约束条件。研究结果为地幔岩浆运移方式和构造板块与岩石圈下地幔之间的应变分配几何结构提供了重要的信息。在这种耦合方法中，具体解决了以下问题：1)伊豆-波宁俯冲带上地幔各向异性的三维分布及其对应变分配和地幔流动的影响；2)地震各向异性结果的解释，特别是它们与地幔运输过程和构造板块与岩石圈下地幔之间耦合程度的关系。该项目的地震部分包括对一组独特的剪切相位进行剪切波分裂分析，包括本地S，远震SKS和sS-S差分分裂。伊豆-博宁地区特别适合拟议的地震研究，因为在伊豆-博宁地区发生的地震提供了一个很好的地震阶段数据集，可以对研究区域的大部分地区进行采样。许多高分辨率地震仪记录了伊豆-波宁地震宽带波形的可用性，并允许约束伊豆-波宁系统各向异性的横向变化和深度分布。该项目的数值模拟部分包括根据一系列物理模型参数计算地幔流动的三维模型。为了确定地幔流动与地震各向异性观测的关系，利用一系列变形研究中适当的弹性参数值，利用流动模型计算预测的各向异性，并将建模结果与地震各向异性结果进行比较。

This study provides new constraints on mantle flow and dynamics within the Izu-Bonin subduction system through a combination of seismic observations and numerical modeling experiments. Results of this work are providing key information regarding mantle processes in convergent margins, including the means of mantle magma transport and the geometry of strain partitioning between tectonic plates and the sublithospheric mantle.In this coupled approach, the following issues are being addressed specifically: 1) the 3-D distribution of upper mantle anisotropy and its implications for strain partitioning and mantle flow in the Izu-Bonin subduction zone; and 2) the interpretation of seismic anisotropy results, particularly their relationship to both mantle transport processes and the degree of coupling between tectonic plates and sublithospheric mantle.The seismic component of the project involves shear wave splitting analysis for a unique set of shear phases, including local S, teleseismic SKS, and sS-S differential splitting. The Izu-Bonin region is particularly well-suited for the proposed seismic studies, as earthquakes generated in Izu-Bonin provide an excellent dataset of seismic phases that sample a broad portion of the study area. The availability of broadband waveforms of Izu-Bonin earthquakes have been recorded by many high-resolution seismographs and allows constraint of both lateral variations and the depth distribution of anisotropy for the Izu-Bonin system. The numerical modeling component of the project involves calculation of 3-D models of mantle flow for a range of physical model parameters. To determine the relationship of mantle flow to the seismic anisotropy observations, flow models are being used to calculate predicted anisotropy using appropriate elastic parameter values from a range of deformation studies, and comparing the modeling results with the seismic anisotropy results.