ORIGINAL ARTICLE
Investigation on Reflection of Tectonic Pattern in ASG EUPOS Data in the Sudetes and Adjacent Areas
1
AGH University of Science and Technology, Faculty of Mining Surveying and Environmental Engineering, Department of Mining Areas Protection, Geoinformatics and Mining Surveying, Poland
Online publication date: 2016-12-30
Publication date: 2016-12-01
Reports on Geodesy and Geoinformatics 2016;102:32-51
KEYWORDS
ABSTRACT
The GNSS data evaluated from on observation of ASG EUPOS stations in the Sudety Mts. and in adjacent areas is analyzed by the author in the scope of disturbances in daily solutions that can be induced by tectonics stress. The daily position changes derived from GNSS data demonstrate the long or short term trends, which are affected by offsets of different nature. Author presents an analysis based on frequency of parameter – displacement vector azimuth. The aim of the analysis is to show statistical significance of observed small values of temporal displacements, which values are not normally distributed. There are “outliers” of the normal distribution of displacement azimuths, which values show a certain reproducibility, which corresponds to orientations of tectonic lines. That suggests small, short time movements along boundaries of horsts and grabens – a crustal-extension structure of the area. However derived results (values of displacements) are less than a limitation error, temporal distributions of coordinates are not random as usually data errors. So in author’s opinion the spatial-temporal evolution of horizontal displacements of ASG EUPOS stations in the Sudety Mts. and in adjacent areas are determined by expressions of underlying geological structures.
REFERENCES (26)
1.
Araszkiewicz A., Bogusz J., Figurski M., Kroszczyński K., Szafranek K. (2009). Report from 30.06.2009 dealing with precise elaboration of observational data from permanent stations of ASG-EUPOS system. The Military Technical Academy. In Polish (Raport z dn. 30.06.2009 r. dotyczący precyzyjnego opracowania danych obserwacyjnych ze stacji permanentnych systemu ASG-EUPOS. Wojskowa Akademia Techniczna). Retrieved from: http://www.asgeupos.pl/webpg/g....
2.
Bogusz J. (2015). Geodetic aspects of GPS permanent station non-linearity studies. Acta Geodyn. Geomater., vol. 12, No. 4 (180), 2015, pp. 323-333, DOI: 10.13168/AGG.2015.0033.
3.
Bogusz J., Figurski M., Kontny B., Grzempowski P.(2012). Horizontal velocity field derived from EPN and ASG-EUPOS satellite data on the example of southwestern part of Poland. Acta Geodynamica et Geomaterialia, vol. 9, No. 3(167), 2012, pp. 349–357.
4.
Bosy J., Graszka W., Leończyk M.(2007)., ASG-EUPOS – a multifunctional precise satellite positioning system in Poland, European Journal of Navigation, Vol. 5 No. 4, Meckenheim, Germany 2007, pp. 30-34.
5.
Brandt S. (1999). Analiza danych. Metody statystyczne i obliczeniowe. Wydawnictwo Naukowe PWN. Warszawa.
6.
Butra J. and Kudełko, J. (2011). Rockburst hazard evaluation and prevention methods in Polish copper mines. Cuprum, 61(4), 2011, pp. 5-20.
7.
Cacoń S., Bosy J., Kontny B. (2004). Recent Tectonic Activity in the Eastern Sudetes and on the Fore-Sudetic Block on the basis of 1993-2003 investigations. Reports on Geodety, Vol. 2 No. 69, Warszawa 2004, pp. 197-211.
8.
Dyjor S. (1993). Etapy blokowego rozwoju Sudetów i ich przedpola w neogenie i starszym czwartorzędzie. Fol. Quatern., 64, Kraków, pp. 25-41. [In Polish].
9.
Figurski M., Szafranek K., Bogusz J., Kamiński P. (2010). Investigation on stability of mountainous EUPOS sites’ coordinates. Acta Geodyn. Geomater., Vol. 7, No. 3 (159), pp. 263–274.
10.
Graniczny M. and Mizerski W. (2003). Lineamenty na zdjęciach satelitarnych Polski – próba podsumowania. Przegląd Geologiczny, Vol. 51, No. 6, pp. 474-482. [In Polish].
11.
Grygar R. and Jellnek J. (2003). The Upper Morava and Nysa pull-apart grabens - the evidence af neotectonic dextral transtension on the Sudetic fault system. Acta Montana. Ser. A. No. 24. Vol. 131, pp. 1-59.
12.
Hefty L. and Gerhátová L. (2012): Potential of precise point positioning using 1 Hz GPS data for detection of seismic-related displacements. Acta Geodynamica et Geomaterialia, Vol. 9, No. 3 (167), pp. 303–313.
13.
Kaczmarek A., Cacoń S and Weigel J. (2016). Recent relative vertical movements in the tectonic zone of the Sudety Mts. Acta Geodyn. Geomater., vol. 13, No. 2 (182), pp. 177-184. DOI: 10.13168/AGG.2015.0055.
14.
Kaczorowski M. and Wojewoda J. (2011). Neotectonic activity interpreted from a long water-tube tiltmeter record at the SRC Geodynamic Laboratory in Ksiaz, Central Sudetes, SW Poland. Acta Geodyn. Geomater., Vol. 8, No. 3 (163), pp. 249–261.
15.
Klos A., Bogusz J., Figurski M., Kosek W. (2015). Irregular variations in the GPS time series by the probability and noise analysis. Survey Review, Vol. 47, Issue 342, pp. 163-173. DOI: 10.1179/1752270614Y.0000000133.
16.
Kontny B. and Bogusz J. (2012). Models of vertical movements of the earth crust surface in the area of Poland derived from leveling and GNSS data. Acta Geodynamica et Geomaterialia, Vol. 9, No. 3 (167), 2012. pp. 331-337.
17.
Kontny B. (2003). Geodezyjne badania współczesnej kinematyki głównych struktur tektonicznych polskich Sudetów i bloku przedsudeckiego na podstawie pomiarów GPS. Zesz. Nauk. AR Wroc. No. 468. Rozprawy, pp. 1-146. [In Polish].
18.
Liszkowski, J.: 1982, The origin of recent vertical crustal movements in Poland. Rozprawy Uniwersytetu Warszawskiego, No. 174, Warszawa, pp. 1-179. [In Polish].
19.
Orlecka-Sikora, B., Papadimitriou, E. E., Kwiatek, G. (2009). A study of the interaction among mining-induced seismic events in the Legnica-Głogów Copper District, Poland. Acta Geophysica, Vol. 57, No. 2, pp. 413-434. https://www.irsm.cas.cz/materi... DOI: 10.2478/s11600-008-0085-z.
20.
Pilecka E. (2007). Statistical analysis of the relation between locations of high energy epicenter tremors and lineaments in areas of the Upper Silesian Basin. Gospodarka Surowcami Mineralnymi, Vol. 23, No. 4. PAN IGSMiE, Kraków, pp. 101-109. [In Polish].
21.
Pilecka E. (2008). An analysis of lineament directions on satellite images in context of the occurrence of an induced seismicity in the Legnica–Głogów Copper District (LGCD). Gospodarka Surowcami Mineralnymi, Vol. 24, No. 2/3. PAN IGSMiE, Kraków, pp. 135–146. [In Polish].
22.
Salski W. (1996). The tectonics of the deposit. In Polish: Tektonika złoża. In: Monografia KGHM Polska Miedź S.A. (editor: A. Piestrzyński). Pub.: Profil, Kraków. [In Polish].
23.
Schenk V. and Schenková Z. (2008). Geodynamic Pattern of the West Bohemia Region based on permanent GPS measurements. Studia geophysica et geodetica, Vol. 53, Issue 3, pp. 329-341. DOI: 10.1007/s11200-009-0021-y.
24.
Szczerbowski Z. and Jura J. (2016). Mining induced seismic events and surface deformations monitored by GPS permanent stations. Acta Geodynamica et Geomaterialia. Vol. 12 No. 3 (179), pp. 237-248. DOI: 10.13168/AGG.2015.0023.
25.
Wojewoda J. (2007). Neotectonic aspect of the intrasudetic shear zone. Acta Geodynamica et Geomaterialia, Vol. 4. No. 4 (148), pp. 31-41.
26.
Znosko J. (1981). The problem of oceanic crust and of ophiolites in the Sudetes. Bull. Acad. Pol. Sc., Ser. Sc. de la Terre, 29, pp. 185–197.
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