Articles | Volume 7, issue 2
https://doi.org/10.5194/se-7-425-2016
https://doi.org/10.5194/se-7-425-2016
Research article
 | 
24 Mar 2016
Research article |  | 24 Mar 2016

POLENET/LAPNET teleseismic P wave travel time tomography model of the upper mantle beneath northern Fennoscandia

Hanna Silvennoinen, Elena Kozlovskaya, and Eduard Kissling

Viewed

Total article views: 3,568 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,866 1,427 275 3,568 253 260 287
  • HTML: 1,866
  • PDF: 1,427
  • XML: 275
  • Total: 3,568
  • Supplement: 253
  • BibTeX: 260
  • EndNote: 287
Views and downloads (calculated since 10 Sep 2015)
Cumulative views and downloads (calculated since 10 Sep 2015)
Latest update: 07 Feb 2026
Download
Short summary
POLENET/LAPNET broadband seismic network was deployed in northern Fennoscandia 2007–2009. In our study we estimate the 3D architecture of the upper mantle beneath the network using high-resolution teleseismic P-wave tomography. Our study reveals a highly heterogeneous lithospheric mantle. The most significant feature seen in the obtained velocity model is a large elongated low-velocity anomaly beneath the crust, separating the three cratonic units that formed the region in the early Proterozoic.
Share