SP12RTS : a degree-12 model of shear- and compressional-wave velocity for Earth's mantle. / Koelemeijer, P.; Ritsema, J.; Deuss, A.; van Heijst, H. J.

In: Geophysical Journal International, Vol. 204, No. 2, 01.02.2016, p. 1024-1039.

Research output: Contribution to journalArticlepeer-review

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Abstract

We present the new model SP12RTS of isotropic shear-wave (V S ) and compressional-wave (V P ) velocity variations in the Earth's mantle. SP12RTS is derived using the same methods as employed in the construction of the shear-wave velocity models S20RTS and S40RTS, and the same data types. SP12RTS includes additional traveltime measurements of P-waves and new splitting measurements: 33 normal modes with sensitivity to the compressional-wave velocity and 9 Stoneley modes with sensitivity primarily to the lowermost mantle. Contrary to S20RTS and S40RTS, variations in V S and V P are determined without invoking scaling relationships. Lateral velocity variations in SP12RTS are parametrised using spherical harmonics up to degree 12, to focus on long-wavelength features of V S and V P and their ratio R. Large-lowvelocity provinces (LLVPs) are observed for both V S and V P . SP12RTS also features an increase of R up to 2500 km depth, followed by a decrease towards the core-mantle boundary. A negative correlation between the shear-wave and bulk-sound velocity variations is observed for both the LLVPs and the surrounding mantle. These characteristics can be explained by the presence of post-perovskite or large-scale chemical heterogeneity in the lower mantle.

Original languageEnglish
Pages (from-to)1024-1039
Number of pages16
JournalGeophysical Journal International
Volume204
Issue number2
Early online date16 Dec 2015
DOIs
Publication statusPublished - 1 Feb 2016
This open access research output is licenced under a Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License.

ID: 34574204