Joint inversion of Rayleigh wave phase velocity and receiver function for estimation of S-wave velocity of deep sedimentary layers in the Kashiwazaki city, Japan
نویسندگان
چکیده
منابع مشابه
Joint inversion of Rayleigh wave phase velocity and ellipticity using USArray: Constraining velocity and density structure in the upper crust
[1] Rayleigh wave ellipticity, or H/V ratio, observed on the surface is particularly sensitive to shallow earth structure. In this study, we jointly invert measurements of Rayleigh wave H/V ratio and phase velocity between 24–100 and 8–100 sec period, respectively, for crust and upper mantle structure beneath more than 1000 USArray stations covering the western United States. Upper crustal stru...
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ژورنال
عنوان ژورنال: BUTSURI-TANSA(Geophysical Exploration)
سال: 2009
ISSN: 0912-7984,1881-4824
DOI: 10.3124/segj.62.237