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Matlab tool REGCONT2: effective source depth estimation by means of Tikhonov’s regularized downwards continuation of potential fields

). Hansen P. C., 2007: Regularization Tools Version 4.0 for Matlab 7.3. Numerical Algorithms 46 , 189–194. Lawson C. L., Hanson R. J., 1974: Solving Least Squares Problems. Prentice-Hall, Englewood Cliffs, 305 p. Li Y., Devriese S. G. R., Krahenbuhl R. A., Davis K., 2013: Enhancement of magnetic data by stable downward continuation for UXO application. IEEE Transactions on Geoscience and Remote Sensing, 51 , 6, 3605–3614. Ma G., Liu C., Huang D., Li L., 2013: A stable iterative downward continuation of potential field data. Journal of Applied

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Applications of Shallow Seismic Refraction Measurements in the Western Carpathians (Slovakia): Case Studies

-808. Park C. B., Xia J., Miller R. D., 1998: Groundroll as a tool to image near surface anomaly. 68th Ann. Internal. Mtg, Soc. Expl. Geophys., Expanded Abstracts, 874-877. Prekopová M., Janočko J., Budinsk´y V., Friedmanov´a M., 2016: Integration of seismic and sedimentological methods for analysis of Quaternary alluvial depositional systems. Environ. Earth Sci. 2017) 76:25, Springer, Reynolds J. M., 1997: An Introduction to Applied and Environmental Geophysics, John Wiley and Sons Ltd, Chichester

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Complex geophysical investigation of the Kapušany landslide (Eastern Slovakia)


Geophysical survey is a very useful and popular tool used by engineering geologists to examine landslides. We present a case study from the Kapušany landslide, Eastern Slovakia, where a broad spectrum of geophysical methods were applied along two perpendicular profiles in order to compare the ability of the methods to detect as many structural features of the landslide as possible. The 2D Electrical Resistivity Tomography inverse model was capable of defining the geological structure of the landslide and defining the shear zone, however the resolution of the inverse model does not allow us to identify cracks or other minor features of the landslide. These, however, were well recorded in the results of Dipole Electromagnetic Imaging and the Self Potential method. In addition microgravimetry, Gamma-Ray Spectrometry and Soil Radon Emanometry were experimentally employed to validate the results obtained from electrical methods and afterwards final geological models, based on the integrated interpretation of all involved methods were constructed.

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Non-observation RINEX compression

References Cormack G., Horspool N., 1987: Data Compression using Dynamic Markov Modelling.Computer Journal, 30:6 (December 1987). Gurtner W., 2002: RINEX: The Receiver Independent Exchange Format Version 2.10. Gurtner W., Estey L., 2009: RINEX. The Receiver Independent Exchange Format. Version3.01. Hatanaka Y., 1996: A RINEX Compression Format and Tools. Proceedings of ION GPS-96

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Relationship between tree bark surface temperature and selected meteorological elements

podmínkách). Zahradnictví, 13 , 5, 8–11 (in Czech). Meier U., 1997: BBCH-Monograph. Growth stages of plants – Entwicklungsstadien von Pflanzen – Estadios de las plantas – Développement des Plantes. Blackwell Wissenschaftsverlag, Berlin und Wien, 622 p. Samietz J., Graf B., Höhn H., Schaub L., Höpli H. U., 2007: Phenology modelling of major insect pests in fruit orchards from biological basics to decision support: the forecasting tool SOPRA*. OEPP/EPPO Bulletin, 37 , 255–260. Středa T., Chuchma F., Rožnovský J., 2011: Abiotic factors of chosen pest

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Inner zone terrain correction calculation using interpolated heights

References Cella F., 2015: GTec-A versatile MATLAB tool for a detailed computation of the terrain correction and Bouguer gravity anomalies. Gomputers & Geosciences 84 , 72–85. Cogbill A. H., 1990: Gravity terrain corrections calculated using digital elevation models. Geophysics, 55 , 1, 102–106. Forsberg R., 1984: A study of terrain reductions, density anomalies and geophysical inversion methods in gravity field modelling. Report no. 5. The Ohio State University. Grand T., Šefara J., Pašteka R., Bielik M., Daniel S., 2001: Atlas of

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The iterative complex demodulation applied on short and long Schumann resonance measured sequences

, 8, 2, 129-144. Madden T., Thompson W., 1964: Low-Frequency Electromagnetic Oscillations in the Earth-Ionosphere Cavity. Res. Rept. Project NR-371-401, Geophysics Laboratory, Cambridge, Mass., 105 p. Mushtak V. C., Williams E. R., 2008: An Improved Lorentzian Technique for Evaluating Resonance Characteristics of Earth-Ionosphere Cavity. Atmospheric Research, doi: 10.1016/j.atmosres.2008.08.013 Myers A. P., Orr D., 1995: ULF Wave Analysis and Complex Demodulation. Proc. of the Cluster Workshop on Data Analysis Tools

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Validation of sensitivity and reliability of GPR and microgravity detection of underground cavities in complex urban settings: Test case of a cellar

Engineering Geology and Hydrogeology, 38 , 155–169. Styles P., Toon S., Thomas E., Skittrall M., 2006: Microgravity as a tool for the detection, characterization and prediction of geohazard posed by abandoned mining cavities. First Break 2, 4 , 51–60. Tuckwell G., Grossey T., Owen S., Stearns P., 2008: The use of microgravity to detect small distributed voids and low-density ground. Quarterly Journal of Engineering Geology and Hydrogeology, 41 , 371–380. Yule D. E., Sharp M. K., Butler D. K., 1998: Microgravity investigations of foundation conditions

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Refined prediction of vertical gradient of gravity at Etna volcano gravity network (Italy)

’area etnea (1986– 1989). Boll. GNV, 5 , 137–146 (in Italian). Carbone D., Greco F., 2007: Review of Microgravity Observations at Mt. Etna: A powerful Tool to Monitor and Study Active Volcanos. Pure Appl. Geophys., 164 , 769–790, doi: 10.1007/s00024-007-0194-7. Carbone D., Poland M. P., Diament M., Greco F., 2017: The added value of time-variable microgravimetry to the understanding of how volcanoes work. Earth-Science Reviews 169 , 146–179, doi: 10.1016/j.earscirev.2017.04.014. Fernández J., Pepe A., Poland M. P., Sigmundsson F., 2017: Volcano Geodesy

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The determination of Schumann resonance mode frequencies using iterative procedure of complex demodulation

. Atmospheric Research, doi:10.1016/j.atmosres.2008.08.013. Myers A. P., Orr D., 1995: ULF Wave Analysis and Complex Demodulation. Proc. of the Cluster Workshop on Data Analysis Tools, Braunschweig, Germany 28 - 30 Sept. 1994 (ESA SP-371, June 1995), 23-32. Nickolaenko A. P., Hayakawa M., 2002: Resonances in the Earth-Ionosphere Cavity, Kluwer Academic Publishers, Dordrecht, 362 p. Ondrásková A., Kostecky P., ň evňík S., Rosenberg L., 2007: Long-term observations of Schumann resonances at Modra Observatory. Radio Sci., 42, RS2S

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