地球与行星物理论评（中英文）2025，Vol.56Issue(3)：313-326,14.DOI:10.19975/j.dqyxx.2024-052
基于接收函数方位变化的青藏高原地壳各向异性研究进展
Review on crustal anisotropy investigations beneath the Qinghai-Xizang Plateau based on azimuthal variations of receiver functions
摘要
Abstract
Seismic anisotropy provides key information about the past and present deformations of the crust and mantle below and is crucial for understanding the interior structure of the Earth and deep dynamic processes.Receiver function is a frequently used method with high lateral resolution to detect velocity discontinuity,composi-tion and anisotropy.In recent years,investigating crustal azimuthal anisotropy based on the azimuthal variations of receiver functions has been widely applied to the study of the uplift and expansion mechanisms of the Qinghai-Xi-zang Plateau.This paper first briefly introduces several main models regarding the uplift and expansion of the Qinghai-Xizang Plateau,the formation mechanisms of seismic anisotropy,and the methods for analyzing crustal anisotropy using receiver functions.Then the recent advances in studying crustal anisotropy of the Qinghai-Xizang Plateau based on the azimuthal variations of receiver functions are introduced in detail.Finally,based on the cur-rent research status,this paper briefly summarizes the challenges and conclusions.Although the formation mecha-nisms of the observed crustal anisotropy remain controversial,these studies provide important observational con-straints on the crustal anisotropy characteristics of the Qinghai-Xizang Plateau and significant implications into its uplift and expansion mechanisms.Based on the high lateral resolution of the receiver function method and an in-creasing number of dense seismic array observations,it is expected that more details of crustal deformation will be observed in the future,which will play a significant role in the study of deep dynamic processes.关键词
青藏高原/接收函数/各向异性/S波分裂/动力学过程Key words
Qinghai-Xizang Plateau/receiver function/seismic anisotropy/S-wave splitting/dynamic process分类
地球科学引用本文复制引用
杨宜海..基于接收函数方位变化的青藏高原地壳各向异性研究进展[J].地球与行星物理论评（中英文）,2025,56(3):313-326,14.基金项目
国家自然科学基金资助项目(42004048) （42004048）
陕西省创新人才推进计划(2022KJXX-22) （2022KJXX-22）
陕西省自然科学基础研究计划资助项目(2024JC-YBMS-219,2020JQ-979)Supported by the National Natural Science Foundation of China(Grant No.42004048),the Innovation Talents Promotion Plan of Shaanxi Province(Grant No.2022KJXX-22),and the Natural Science Basic Research Program of Shaanxi Province(Grant Nos.2024JC-YBMS-219,2020JQ-979) （2024JC-YBMS-219,2020JQ-979）
