Shear wave crustal velocity model of the Western Bohemian Massif from Love wave phase velocity dispersion
نویسندگان
چکیده
منابع مشابه
Empirical relation for estimating shear wave velocity from compressional wave velocity of rocks
In situ shear wave velocity is one of the most important parameters for evaluating dynamic elastic moduli and needs special energy sources for generation and receivers for detection. Identification of shear wave phase on a seismic record needs skill as it is not the first wave to arrive and is usually embedded in surface waves. To estimate shear wave velocity for site characterization and for p...
متن کاملCrustal shear wave velocity structure of the western United States inferred from ambient seismic noise and earthquake data
[1] Surface wave dispersion measurements from ambient seismic noise and array‐based measurements from teleseismic earthquakes observed with the EarthScope/USArray Transportable Array (TA) are inverted using a Monte Carlo method for a 3‐D VS model of the crust and uppermost mantle beneath the western United States. The combination of data from these methods produces exceptionally broadband dispe...
متن کاملCrustal shear velocity structure of the western US
F.-C. Lin, Center for Imaging the Earth’s Interior, Department of Physics, University of Colorado, 390 UCB, Boulder, CO, 80390-0390, USA. ([email protected]) M. P. Moschetti, Center for Imaging the Earth’s Interior, Department of Physics, University of Colorado, 390 UCB, Boulder, CO, 80390-0390, USA. ([email protected]) M. H. Ritzwoller, Center for Imaging the Earth’s Interior, D...
متن کاملRegional Ambient Noise Tomography in the Eastern Alps of Europe
We present results from ambient noise tomography applied to temporary seismological stations in the easternmost part of the Alps and their transition to the adjacent tectonic provinces (Vienna Basin, Bohemian Massif, Southern Alps, Dinarides). By turning each station into a virtual source, we recover surface waves in the frequency range between 0.1 and 0.6 Hz, which are sensitive to depths of a...
متن کاملAverage shear-wave velocity structure of the Kamchatka peninsula from the dispersion of surface waves
An average shear-wave velocity structure has been estimated for the path between the Kamchatka Isthmus and Petropavlovsk-Kamchatski. It is obtained from the Monte Carlo inversion of the Rayleigh and Love wave group velocity dispersion curves measured using broad-band seismograms of events in Northern Kamchatka recorded by the IRIS station PET in Petropavlovsk-Kamchatski. The Moho interface was ...
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ژورنال
عنوان ژورنال: Journal of Seismology
سال: 2010
ISSN: 1383-4649,1573-157X
DOI: 10.1007/s10950-010-9209-4