首页|一种有效的适合F-J方法从背景噪声资料中提取多阶频散曲线的台阵划分方法

一种有效的适合F-J方法从背景噪声资料中提取多阶频散曲线的台阵划分方法

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近年发展起来的从地震背景噪声提取多阶频散曲线的F-J方法是一种台阵分析方法,对某一特定的研究区域内台阵的划分方式直接影响成像的效果.当研究区域地下结构较简单,且台站间距比较均匀时,可以使用简单的平移式移动阵列法;然而若研究区域地下结构复杂多变,尤其是台站间距疏密不均时,就需要根据具体的地域特征灵活划分台阵.本文介绍了一种适用于地下结构复杂及台站间距不均匀区域的台阵划分方法,具有一定的普适性.我们将其应用于美国阿拉斯加及加拿大西北部,验证了相比于简单的沿经纬度移动阵列,我们的分区方法确实大大提高了结果的分辨率,为后续反演研究区域三维速度结构提供了坚实的保障.
Efficient array partitioning method for F-J transform to extract multimode dispersion curves from ambient noise data
The recently developed F-J transform method relies on the array configuration of seismic stations,which directly affects the imaging results of the velocity structure beneath a specific study area.When the underground structure of the study area varies gently and the station spacing is relatively uniform,it is sufficient to simply move a fixed-size rectangular box gradually along the latitude and longitude.However,if the subsurface structure of the study area is complex and variable,especially when the station spacing is uneven,the array needs to be divided flexibly according to the specific geographical features.This paper introduces an array partitioning method suitable for regions characterized by complex subsurface structures and non-uniform station spacing,exhibiting a certain level of generality.By applying this method to the Alaskan and northwestern Canadian regions,we have validated that our partitioning approach significantly enhances the resolution of the results compared to the simplistic latitude and longitude-based moving array method.This improvement provides a solid foundation for subsequent inversion studies aiming to investigate the three-dimensional velocity structure of the research area.

F-J transformArray partitioning methodMulti-mode surface waveAlaska

袁艺、陈晓非

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北京大学地球与空间科学学院,北京 100871

中国地震局第二监测中心,西安 710054

广东省地球物理高精度成像技术重点实验室(南方科技大学),深圳 518055

南方科技大学地球与空间科学系,深圳 518055

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F-J变换 台阵划分方法 多阶面波 阿拉斯加

国家自然科学基金资助项目广东省地球物理高精度成像技术重点实验室深圳市科技计划资助

U19016022022B1212010002KQTD20170810111725321

2024

地球物理学报
中国地球物理学会 中国科学院地质与地球物理研究所

地球物理学报

CSTPCD北大核心
影响因子:3.703
ISSN:0001-5733
年,卷(期):2024.67(2)
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