Anisotropic lithosphere under the Fennoscandian shield from P receiver functions and SKS waveforms of the POLENET/LAPNET array

Seismic azimuthal anisotropy is the key evidence of the past and present strains in the upper mantle. The standard analysis of shear-wave splitting with the SKS techniques is useful in mapping lateral variations but it is insensitive to depth of anisotropy and to variations of anisotropy with depth....

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Bibliographic Details
Published in:Tectonophysics
Main Authors: Vinnik, L., Oreshin, S., Makeyeva, L., Peregoudov, D., Kozlovskaya, E., Pedersen, H., Plomerová, J. (Jaroslava), Achauer, U., Kissling, E., Sanina, I., Jämsen, T., Silvennoinen, H., Pequegnat, C., Hurskainen, R., Guiguet, R., Hausmann, H., Jedlička, P. (Petr), Aleshin, I., Bourova, E., Bodvarsson, R., Brückl, E., Eken, T., Heikkinen, P., Houseman, G., Johnsen, H., Kremenetskaya, E., Komminaho, K., Munzarová, H. (Helena), Roberts, R., Růžek, B. (Bohuslav), Shomali, H., Schweitzer, J., Shaumyan, A., Vecsey, L. (Luděk), Volosov, S.
Format: Article in Journal/Newspaper
Language:English
Published: 2014
Subjects:
lithosphere
asthenosphere
seismic anisotropy
mantle flow
receiver functions
shear-wave splitting
Fennoscandian
Northern Finland
Online Access:https://doi.org/10.1016/j.tecto.2014.04.024
http://hdl.handle.net/11104/0237414
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Summary:Seismic azimuthal anisotropy is the key evidence of the past and present strains in the upper mantle. The standard analysis of shear-wave splitting with the SKS techniques is useful in mapping lateral variations but it is insensitive to depth of anisotropy and to variations of anisotropy with depth. To retrieve the depth localized anisotropy under the Fennoscandian shield, we inverted P-wave receiver functions of the POLENET/LAPNET array in northern Finland jointly with SKS recordings. Shear-wave anisotropy of similar to 2.5% with the fast direction of 40 degrees-60 degrees in a depth range from the Moho to similar to 110 km is a robust result of the inversion. The obtained direction is nearly normal to the azimuth of the maximum horizontal compressional stress in the lithosphere, but a recent origin of this anisotropy is in doubt. This anisotropy may be frozen since the Precambrian, but it shows no clear relation with the trends of the Precambrian tectonics. The upper anisotropic layer accounts for similar to 40% of shear-wave splitting in SKS, and to explain the rest another anisotropic layer is required.

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