地球与行星物理论评（中英文）2025，Vol.56Issue(5)：514-527,14.DOI:10.19975/j.dqyxx.2025-020
地震干涉自相关成像方法及应用进展
Research progress on the seismic interferometric auto-correlation imaging method
摘要
Abstract
The seismic interferometric auto-correlation imaging method reconstructs virtual zero-offset reflec-tion response beneath a single seismic station by stacking the auto-correlation of earthquakes or ambient noise.This technique has gained increasing attention for its capability to image Earth's interior structures,and has also been ex-tended to studies of the Moon and the Mars.Relying solely on single-station records,it circumvents the need for inter-station synchronization and allows imaging using single component seismic data,enhancing operational flexi-bility.The auto-correlation imaging method,also known as the generalized receiver function or vertical receiver function,offers distinct advantages over conventional receiver functions.By utilizing frequency components with higher and broader-bandwidth from earthquakes or ambient noise,it achieves improved vertical resolution for ima-ging subsurface discontinuities.Moreover,it is less affected by multiple scattering phases,enhancing its robustness in complex geological environments.This method has been used to efficiently identify the major discontinuities in the Earth's interior,including the Moho,mid-lithospheric discontinuity,Hales discontinuity,lithosphere-astheno-sphere boundary,and Lehmann discontinuity.In addition,it has been used to probe the anisotropy of the Earth's in-ner core.First,we briefly summarize the historical development of the auto-correlation imaging method.Second,we focus on its fundamental principles and processing workflows.Spectral whitening plays a key role in improving the auto-correlation imaging results.Phase-weighted stacking is a valuable procedure to enhance the signal-to-noise ratio and help to more easily identify weak yet important reflections with high coherence.Third,we outline recent advances in applications involving global,teleseismic,regional,and local earthquake events,as well as ambient noise in more detail.In the end,key challenges and potential solutions are discussed,and future directions are ex-plored in the context of emerging trends in earthquake seismology.关键词
地震干涉/背景噪声/自相关/互相关/天然地震/接收函数Key words
seismic interferometry/ambient noise/auto-correlation/cross-correlation/earthquake/receiver function分类
天文与地球科学引用本文复制引用
杨积忠,周雨琪,卢柱峰..地震干涉自相关成像方法及应用进展[J].地球与行星物理论评（中英文）,2025,56(5):514-527,14.基金项目
国家自然科学基金资助项目(42374136) （42374136）
中央高校基本科研业务费专项资金(22120230311) （22120230311）
同济大学海洋交叉平台项目(2023-1-YB-03)Supported by the National Natural Science Foundation of China(Grant No.42374136),the Fundamental Research Funds for the Central Universities(Grant No.22120230311),and the Interdisciplinary Project in Ocean Research of Tongji University(Grant No.2023-1-YB-03) （2023-1-YB-03）
