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Solid Earth An interactive open-access journal of the European Geosciences Union
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Volume 2, issue 2
Solid Earth, 2, 303-313, 2011
https://doi.org/10.5194/se-2-303-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: The Lithosphere-Asthenosphere Boundary (LAB) Dilemma

Solid Earth, 2, 303-313, 2011
https://doi.org/10.5194/se-2-303-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 15 Dec 2011

Research article | 15 Dec 2011

Domains of Archean mantle lithosphere deciphered by seismic anisotropy – inferences from the LAPNET array in northern Fennoscandia

J. Plomerová, L. Vecsey, V. Babuška, and LAPNET Working Group J. Plomerová et al.
  • Geophysical Institute, Academy of Science of the Czech Republic, Boční II/1401, 141 31 Prague, Czech Republic

Abstract. An international LAPNET array (2007–2009, http://www.oulu.fi/sgo-oty/lapnet) of the POLENET/LAPNET sub-project of the POLENET-IPY consortium, related to seismic and geodetic studies in the Arctic regions, consisted of about 60 broadband seismic stations located on the territory of northern Finland and adjacent parts of Sweden, Norway and Russia. We analyze relative P-wave travel-time deviations evaluated for a subset of 90 teleseismic events recorded by the LAPNET array and show examples of lateral variations of shear-wave splitting to demonstrate variability of fabrics of the Archean mantle lithosphere. The initial results clearly demonstrate the Archean mantle lithosphere consists of domains with consistent fabrics reflecting fossil anisotropic structures. 3-D self-consistent anisotropic models with inclined symmetry axes accommodate two independent sets of body-wave anisotropic observations. Individual domains are delimited by boundaries (sutures), where the anisotropic parameters change. The results obtained from the LAPNET array fill a gap in structural studies of the upper mantle beneath northern Fennoscandia.

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