One major cause of elastic wave attenuation in heterogeneous porous media is wave-
induced flow of the pore fluid between heterogeneities of various scales. It is believed that …

With the emergence of portable broadband seismic instrumentation, availability of digital
networks with wide dynamic range, and development of new powerful analysis techniques …

Using data from more than 2000 seismic stations from multiple networks arrayed throughout
China (CEArray, China Array, NECESS, PASSCAL, GSN) and surrounding regions (Korean …

This paper presents a new model of the shear velocity structure of the crust and uppermost
mantle beneath the contiguous US The model is based on more than a decade of USArray …

It has been widely recognized that the cross‐correlation function of ambient seismic noise
data recorded at two stations approximates to the part of Greens function between two …

Ambient noise tomography has proven to be effective in resolving shallow earth structure.
We applied ambient noise tomography on a dense seismic array in Long Beach, California …

We propose a method to invert surface wave dispersion data directly for 3-D variations of
shear wave speed, that is, without the intermediate step of phase or group velocity maps …

The water cycle at subduction zones remains poorly understood, although subduction is the
only mechanism for water transport deep into Earth. Previous estimates of water flux,–exhibit …

Seismic interferometry involves the crosscorrelation of responses at different receivers to
obtain the Green's function between these receivers. For the simple situation of an impulsive …

In optical coherence elastography, images are formed by map** a mechanical property of
tissue. Such images, known as elastograms, are formed on the microscale, intermediate …