节点文献
S波接收函数方法研究进展
Review of the s-wave receiver function method
【摘要】 近年来发展起来的S波接收函数方法在探测岩石圈-软流圈边界(LAB)和岩石圈地幔速度结构方面显示了明显优势.本文详细介绍了S波接收函数的提取、S波接收函数偏移成像方法、P波和S波接收函数联合反演方法的相关理论及数据处理流程;概括总结了近年来应用该方法取得的一些重要研究成果;讨论了目前S波接收函数方法遇到的问题和发展前景.
【Abstract】 The S receiver functions( SRF) method developed in recent years has appeared great advantage for studying lithosphereasthenosphere boundary( LAB) and mantle lithosphere velocity structure. The relative theory and data processing about the SRF extracting,the SRF migration imaging technique,PRF and SRF joint inversion technique are introduced in detail. Some important studying results obtained by using SRF technique are summarized.This paper finally discusses the problems and prospects on SRF technique in further development.
【关键词】 S波接收函数;
岩石圈底部边界;
岩石圈地幔速度结构;
偏移成像;
联合反演;
【Key words】 S receiver functions; LAB; mantle lithosphere velocity structure; migration imaging technique; joint inversion;
【Key words】 S receiver functions; LAB; mantle lithosphere velocity structure; migration imaging technique; joint inversion;
【基金】 国家自然科学基金(41304039);中国地震局地震预测研究所基本科研业务专项(2014IES0405;2010IES010103)共同资助
- 【文献出处】 地球物理学进展 ,Progress in Geophysics , 编辑部邮箱 ,2016年01期
- 【分类号】P315.6
- 【被引频次】2
- 【下载频次】305