东京火山岛自然地震层析成像的棋盘解析度测试

Kentaro Omori, Y. Oda
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引用次数: 0

摘要

在以单一火山为目标的自然地震层析成像中,一般采用临时地震观测来提高分辨率。但是,由于观测点数量和观测周期有限,因此提前掌握假定分辨率非常重要。因此,在对东京火山岛八丈岛、小竹岛和新岛进行自然地震层析成像时,采用棋盘分辨率试验(CRT)的数值实验方法,考察了通过临时地震观测,以多少个观测点和观测周期(地震次数)估算地下速度结构的分辨率。CRT是显示自然地震层析成像分辨率和评价分辨率较好的参数(一对网格点间距、观测点和地震次数)对分辨率影响的合理方法之一。使用CRT进行参数化研究的结果发现,在我所研究的每一个岛屿上,当设置一对一定的网格点间距、一定数量的观测点和一定数量的地震时,它们都可以以一定的分辨率成像。考虑到未来将在东京火山岛进行临时地震观测,本研究获得的数据对于制定观测计划非常重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Checkerboard resolution test for natural earthquake tomography of volcanic islands in Tokyo
In natural earthquake tomography targeting a single volcano, temporary seismic observation is carried out in order to improve resolution in general. However, since the number of observation points and observation period are limited, it is important to grasp the presumable resolution in advance. Therefore, we conducted to examine how much resolution we can estimate the underground velocity structure by performing temporary seismic observation with how many observation points and observation period (the number of earthquakes), when carrying out natural seismic tomography on Hachijojima, Kozushima and Niijima of volcanic islands in Tokyo by using numerical experiments, a checkerboard resolution test (CRT). CRT is one of the reasonable tests to show the resolution of the natural earthquake tomography and to evaluate the influence of parameters with good resolution (a pair of grid point spacing, observation points and number of earthquakes) on the resolution. As the results of parametric study using CRT, we have found that in every island I have researched, when setting a pair of some grid point spacing, some number of observation points and some number of earthquakes, they were possible to image with a resolution of some degree. Considering that temporary seismic observation will be carried out in volcanic islands, Tokyo, in the future, the data obtained in this study will be very important for establishing the observation plan.
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