Articles | Volume 12, issue 7
https://doi.org/10.5194/se-12-1563-2021
https://doi.org/10.5194/se-12-1563-2021
Research article
 | 
07 Jul 2021
Research article |  | 07 Jul 2021

Near-surface structure of the Sodankylä area in Finland, obtained by passive seismic interferometry

Nikita Afonin, Elena Kozlovskaya, Suvi Heinonen, and Stefan Buske

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Improving the quality of empirical Green's functions, obtained by cross-correlation of high-frequency ambient seismic noise
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Subject area: Crustal structure and composition | Editorial team: Seismics, seismology, paleoseismology, geoelectrics, and electromagnetics | Discipline: Geophysics
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Cited articles

Åberg, A. K., Salonen, V. P., Korkka-Niemi, K., Rautio, A., Koivisto, E., and Åberg, S. C.: GIS-based 3D sedimentary model for visualizing complex glacial deposition in Kersilö, Finnish Lapland, Boreal Environ. Res., 22, 277–298, 2017. 
Abraham, E. M. and Alile, O. M.: Modelling subsurface geologic structures at the Ikogosi geothermal field, southwestern Nigeria, using gravity, magnetics and seismic interferometry techniques, J. Geophys. Eng., 16, 729–741, https://doi.org/10.1093/jge/gxz034, 2019. 
Afonin, N., Kozlovskaya, E., Kukkonen, I., and DAFNE/FINLAND Working Group: Structure of the Suasselkä postglacial fault in northern Finland obtained by analysis of local events and ambient seismic noise, Solid Earth, 8, 531–544, https://doi.org/10.5194/se-8-531-2017, 2017. 
Afonin, N., Kozlovskaya, E., Nevalainen, J., and Narkilahti, J.: Improving the quality of empirical Green's functions, obtained by cross-correlation of high-frequency ambient seismic noise, Solid Earth, 10, 1621–1634, https://doi.org/10.5194/se-10-1621-2019, 2019. 
Aki, K.: Analysis of the seismic coda of local earthquakes as scattered waves, J. Geophys. Res., 74, 615–631, 1969. 
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Short summary
In our study, we show the results of a passive seismic interferometry application for mapping the uppermost crust in the area of active mineral exploration in northern Finland. The obtained velocity models agree well with geological data and complement the results of reflection seismic data interpretation.