Traditional methods of imaging the Earth's subsurface using seismic waves require an
identifiable, impulsive source of seismic energy, for example an earthquake or explosive …

The term seismic interferometry refers to the principle of generating new seismic responses
by crosscorrelating seismic observations at different receiver locations. The first version of …

Seismic interferometry is an exciting new field in geophysics utilizing multiple scattering
events to provide unprecedented views of the Earth's subsurface. This is the first book to …

Classical seismological receiver functions are correlational or deconvolutional combinations
of vertical and horizontal component seismometer recordings of earthquake waves that …

基于背景噪声的地震方法发展迅速, 已广泛应用于全球和区域地球内部结构研究,
浅地表地质调查及油气田勘探开发. 本文简要介绍了背景噪声的来源, 回顾了噪声地震学的发展 …

Seismic interferometry applied to 120 hr of railroad traffic recorded by an array of vertical
component seismographs along a railway within the Rio Grande rift has recovered surface …

Interferometry allows for synthesis of data recorded at any two receivers into waves that
propagate between these receivers as if one of them behaves as a source. This is …

Shear-wave splitting provides insight into geodynamic processes such as lithospheric
deformation and upper mantle flow. This study presents shear wave splitting parameters …

Deconvolution interferometry successfully recovers the impulse response between two
receivers without the need for an independent estimate of the source function. Here we …

Waves generated by opportunistic or ambient noise sources and recorded by passive
sensor arrays can be used to image the medium through which they travel. Spectacular …