S40RTS: a degree-40 shear-velocity model for the mantle from new Rayleigh wave dispersion, teleseismic traveltime and normal-mode splitting function measurements

We have developed model S40RTS of shear-velocity variation in Earth's mantle using a new collection of Rayleigh wave phase velocity, teleseismic body-wave traveltime and normal-mode splitting function measurements. This data set is an order of magnitude larger than used for S20RTS and includes...

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Bibliografski detalji
Glavni autori: Ritsema, J, Deuss, A, van Heijst, H, Woodhouse, J
Format: Journal article
Jezik:English
Izdano: 2011