Articles | Volume 7, issue 2
https://doi.org/10.5194/se-7-425-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/se-7-425-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
POLENET/LAPNET teleseismic P wave travel time tomography model of the upper mantle beneath northern Fennoscandia
Hanna Silvennoinen
CORRESPONDING AUTHOR
Sodankylä Geophysical Observatory, University of Oulu, P.O. Box
3000, 90014 Oulu, Finland
Elena Kozlovskaya
Oulu Mining School, University of Oulu,
P.O. Box 3000, 90014 Oulu, Finland
Sodankylä Geophysical Observatory, University of Oulu, P.O. Box
3000, 90014 Oulu, Finland
Eduard Kissling
Institute of Geophysics, ETH
Zürich, Sonneggstrasse 5, 8092 Zürich, Switzerland
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Cited
14 citations as recorded by crossref.
- Thermochemical Heterogeneity and Density of Continental and Oceanic Upper Mantle in the European‐North Atlantic Region A. Shulgin & I. Artemieva 10.1029/2018JB017025
- Novel anisotropic teleseismic body-wave tomography code AniTomo to illuminate heterogeneous anisotropic upper mantle: Part I — Theory and inversion tuning with realistic synthetic data H. Munzarová et al. 10.1093/gji/ggy296
- Novel anisotropic teleseismic body-wave tomography code AniTomo to illuminate heterogeneous anisotropic upper mantle: Part II – Application to data of passive seismic experiment LAPNET in northern Fennoscandia H. Munzarová et al. 10.1093/gji/ggy327
- Lithosphere structure in Europe from thermal isostasy I. Artemieva 10.1016/j.earscirev.2018.11.004
- Seismic observations at the Sodankylä Geophysical Observatory: history, present, and the future E. Kozlovskaya et al. 10.5194/gi-5-365-2016
- The Modern Swedish National Seismic Network: Two Decades of Intraplate Microseismic Observation B. Lund et al. 10.1785/0220200435
- Two subduction-related heterogeneities beneath the Eastern Alps and the Bohemian Massif imaged by high-resolution P-wave tomography J. Plomerová et al. 10.5194/se-13-251-2022
- Studying local earthquakes in the area Baltic-Bothnia Megashear using the data of the POLENET/LAPNET temporary array O. Usoltseva & E. Kozlovskaya 10.5194/se-7-1095-2016
- Highly heterogeneous upper-mantle structure in Fennoscandia from finite-frequency P-body-wave tomography N. Bulut et al. 10.1093/gji/ggac107
- The Mid‐Lithospheric Discontinuity Caused by Channel Flow in Proto‐Cratonic Mantle H. Yang et al. 10.1029/2022JB026202
- Characteristics of Radiation and Propagation of Seismic Waves in Northern Finland, Estimated Based on Records of Local Earthquakes O. Pavlenko & E. Kozlovskaya 10.1007/s00024-018-1919-5
- ScanArray—A Broadband Seismological Experiment in the Baltic Shield H. Thybo et al. 10.1785/0220210015
- A shear-wave velocity model for the Scandinavian lithosphere from Rayleigh waves and ambient noise - Implications for the origin of the topography of the Scandes mountain range A. Mauerberger et al. 10.1016/j.tecto.2022.229507
- Studying local earthquakes in the northern Fennoscandian Shield using the data of the POLENET/LAPNET temporary array O. Usoltseva & E. Kozlovskaya 10.5194/sed-7-3689-2015
13 citations as recorded by crossref.
- Thermochemical Heterogeneity and Density of Continental and Oceanic Upper Mantle in the European‐North Atlantic Region A. Shulgin & I. Artemieva 10.1029/2018JB017025
- Novel anisotropic teleseismic body-wave tomography code AniTomo to illuminate heterogeneous anisotropic upper mantle: Part I — Theory and inversion tuning with realistic synthetic data H. Munzarová et al. 10.1093/gji/ggy296
- Novel anisotropic teleseismic body-wave tomography code AniTomo to illuminate heterogeneous anisotropic upper mantle: Part II – Application to data of passive seismic experiment LAPNET in northern Fennoscandia H. Munzarová et al. 10.1093/gji/ggy327
- Lithosphere structure in Europe from thermal isostasy I. Artemieva 10.1016/j.earscirev.2018.11.004
- Seismic observations at the Sodankylä Geophysical Observatory: history, present, and the future E. Kozlovskaya et al. 10.5194/gi-5-365-2016
- The Modern Swedish National Seismic Network: Two Decades of Intraplate Microseismic Observation B. Lund et al. 10.1785/0220200435
- Two subduction-related heterogeneities beneath the Eastern Alps and the Bohemian Massif imaged by high-resolution P-wave tomography J. Plomerová et al. 10.5194/se-13-251-2022
- Studying local earthquakes in the area Baltic-Bothnia Megashear using the data of the POLENET/LAPNET temporary array O. Usoltseva & E. Kozlovskaya 10.5194/se-7-1095-2016
- Highly heterogeneous upper-mantle structure in Fennoscandia from finite-frequency P-body-wave tomography N. Bulut et al. 10.1093/gji/ggac107
- The Mid‐Lithospheric Discontinuity Caused by Channel Flow in Proto‐Cratonic Mantle H. Yang et al. 10.1029/2022JB026202
- Characteristics of Radiation and Propagation of Seismic Waves in Northern Finland, Estimated Based on Records of Local Earthquakes O. Pavlenko & E. Kozlovskaya 10.1007/s00024-018-1919-5
- ScanArray—A Broadband Seismological Experiment in the Baltic Shield H. Thybo et al. 10.1785/0220210015
- A shear-wave velocity model for the Scandinavian lithosphere from Rayleigh waves and ambient noise - Implications for the origin of the topography of the Scandes mountain range A. Mauerberger et al. 10.1016/j.tecto.2022.229507
Saved (final revised paper)
Latest update: 27 Mar 2024
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.
POLENET/LAPNET broadband seismic network was deployed in northern Fennoscandia 2007–2009. In...
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