Results 261 to 270 of about 48,466 (293)
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Shear-wave splitting observations on Milos, Greece

Geothermics, 1989
Abstract Seismograms from local earthquakes recorded on Milos have been analysed for shear-wave splitting diagnostic of seismic anisotropy. Many complex P- and shear-wave trains were observed, indicating the presence of much heterogeneity, but shear-wave splitting was identified in most shear-wave arrivals within the shear-wave window.
D.C. Booth   +4 more
openaire   +1 more source

Shear Wave Splitting Analysis Using SKS Phase

Proceedings, 2018
Summary Anisotropy is an intrinsic part of our real Earth and the simplified assumption of an isotropic subsurface is generally not satisfied. Seismic anisotropy is mostly indicated by splitting of shear waves. We have worked on two earthquake events from the Andaman and Nicobar Islands and performed anisotropic correction for the two events by ...
T. Dev, P. Kumar
openaire   +1 more source

Shear wave splitting and subcontinental mantle deformation

Journal of Geophysical Research: Solid Earth, 1991
We have made measurements of shear wave splitting in the phases SKS and SKKS at 21 broadband stations in North America, South America, Europe, Asia, and Africa. Measurements are made using a retrieval scheme that yields the azimuth of the fast polarization direction ϕ and delay time δt of the split shear wave plus uncertainties.
Paul G. Silver, W. Winston Chan
openaire   +1 more source

A New Understanding of Shear-Wave Splitting

Proceedings, 1995
Shear-wave splitting (shear-wave- bi-refringence) diagnostic of some form of azimuthal anisotropy is widely observed in all types of rock in the uppermost 15km of the Earth's crust (Crampin and Lovell 1991).
S. Crampin, S. V. Zatsepin
openaire   +1 more source

Error in shear‐wave polarization and time splitting

Geophysical Prospecting, 2004
ABSTRACTShear‐wave polarization and time delay are attributes commonly used for fracture detection and characterization. In time‐lapse analysis these parameters can be used as indicators of changes in the fracture orientation and density. Indeed, changes in fracture characteristics provide key information for increased reservoir characterization and ...
Gwénola Michaud, Roel Snieder
openaire   +1 more source

Shear‐wave splitting in cross‐hole surveys: Modeling

GEOPHYSICS, 1989
Shear‐wave splitting, diagnostic of some form of effective seismic anisotropy, is observed along almost all near‐vertical raypaths through the crust. The splitting is caused by propagation through distributions of stress‐aligned vertical parallel fluid‐filled cracks, microcracks, and preferentially oriented pore space that exist in most crustal rocks.
Enru Liu, Stuart Crampin, David C. Booth
openaire   +1 more source

Evaluation of anisotropy by shear‐wave splitting

GEOPHYSICS, 1985
The polarizations of three‐component shear wavetrains carry unique information about the internal structure of the rock through which they pass: specifically, commonly observed shear‐wave splitting may contain information about the orientation of crack distributions.
openaire   +1 more source

Analysis of Shear-Wave Splitting

66th EAGE Conference & Exhibition, 2004
K. Henneberg, J. Langhammer, T. Tvedt
openaire   +1 more source

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