Crust Macrofracturing as the Evidence of the Last Deglaciation
Author:
Funder
Ministry of Science and Higher Education of the Russian Federation
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
https://link.springer.com/content/pdf/10.1007/s00024-023-03334-7.pdf
Reference38 articles.
1. Aleshin, I., Kosarev, G., Riznichenko, O., & Sanina, I. (2006). Crustal velocity structure under the RUKSA seismic array (Karelia, Russia). Russian Journal of Earth Sciences, 8, 1–8. https://doi.org/10.2205/2006ES000194
2. Aleshin, I., Vaganova, N., Kosarev, G., & Malygin, I. (2019). The crust properties in fennoscandia resulted from knn-analysis of receiver function inversions (in Russian). Geophysical Research, 20(4), 25–39. https://doi.org/10.21455/gr2019.4-2
3. Alinaghi, A., Bock, G., Kind, R., Hanka, W., Wylegalla, K., TOR, Groups, S.W. (2003). Receiver function analysis of the crust and upper mantle from the North German Basin to the Archaean Baltic Shield. Geophysical Journal International, 155(2), 641–652. https://doi.org/10.1046/j.1365-246X.2003.02075.x
4. Bock, G., Achauer, U., Alinaghi, A., Ansorge, J., Bruneton, M., Friederich, W., & Kissling, E. (2001). Seismic probing of fennoscandian lithosphere. Eos, Transactions American Geophysical Union, 82, 621–621. https://doi.org/10.1029/01EO00356
5. Bruneton, M., Farra, V., & Pedersen, H. A. (2002). Non-linear surface wave phase velocity inversion based on ray theory. Geophysical Journal International, 151(2), 583–596. https://doi.org/10.1046/j.1365-246X.2002.01796.x
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