Seismic Interferometry: Tutorial on seismic interferometry: Part 1—Basic principles and applications
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 …
obtain the Green's function between these receivers. For the simple situation of an impulsive …
Seismic anisotropy beneath stable continental interiors
MJ Fouch, S Rondenay - Physics of the Earth and Planetary Interiors, 2006 - Elsevier
A robust knowledge of seismic anisotropy beneath the continents is essential to our
understanding of plate tectonic theory, as anisotropy provides a unique constraint on the …
understanding of plate tectonic theory, as anisotropy provides a unique constraint on the …
[图书][B] Seismic wave propagation and scattering in the heterogeneous earth
The structure of the earth has been extensively studied using seismic waves generated by
natural earthquakes and man-made sources. In classical seismology, the earth is …
natural earthquakes and man-made sources. In classical seismology, the earth is …
Green's function representations for seismic interferometry
K Wapenaar, J Fokkema - Geophysics, 2006 - library.seg.org
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 …
by crosscorrelating seismic observations at different receiver locations. The first version of …
An inverted continental Moho and serpentinization of the forearc mantle
Volatiles that are transported by subducting lithospheric plates to depths greater than 100
km are thought to induce partial melting in the overlying mantle wedge, resulting in arc …
km are thought to induce partial melting in the overlying mantle wedge, resulting in arc …
Full waveform tomography for lithospheric imaging: results from a blind test in a realistic crustal model
AJ Brenders, RG Pratt - Geophysical Journal International, 2007 - academic.oup.com
A comprehensive validation of 2-D, frequency-domain, acoustic wave-equation tomography
was undertaken in a 'blind test', using third-party, realistic, elastic wave-equation data. The …
was undertaken in a 'blind test', using third-party, realistic, elastic wave-equation data. The …
Changes in dip of subducted slabs at depth: petrological and geochronological evidence from HP–UHP rocks (Tianshan, NW-China)
High-resolution seismic imaging has previously revealed sudden changes in the dip of
subducted oceanic plates. This 'kinking'feature is crucial because in many subduction zones …
subducted oceanic plates. This 'kinking'feature is crucial because in many subduction zones …
Thermal–petrological controls on the location of earthquakes within subducting plates
We find that in young and warm subducting plates, earthquakes occur just below the Moho.
In older plates, earthquakes occur throughout the subducting oceanic crust, as well as the …
In older plates, earthquakes occur throughout the subducting oceanic crust, as well as the …
Mantle wedge water contents estimated from seismic velocities in partially serpentinized peridotites
RL Carlson, DJ Miller - Geophysical Research Letters, 2003 - Wiley Online Library
Water carried into subduction zones with the down‐going plate and subsequently released
by dehydration reactions at depth affects the composition of the mantle wedge, triggers …
by dehydration reactions at depth affects the composition of the mantle wedge, triggers …
High resolution image of the subducted Pacific (?) plate beneath central Alaska, 50–150 km depth
A Ferris, GA Abers, DH Christensen… - Earth and Planetary …, 2003 - Elsevier
A receiver function transect across the Alaska Range images the subducting Pacific plate at
50–150 km depth. Across a 200 km long array of 30 receivers, the largest observed P-to-S …
50–150 km depth. Across a 200 km long array of 30 receivers, the largest observed P-to-S …