Research of horizontal movements of the earth's crust in the Archipelago Argentine Islands (Antarctica) during period 2003-2018

Geodesy, Architecture & Construction
Proceedings of the 8th International Youth Science Forum "Litteris et Artibus", November 22–24, 2018, Lviv: Lviv Polytechnic National University, 2018, pp. 37–40

Authors

First and Last Name Academic degree E-mail Affiliation
Ihor Savchyn Ph.D. savchyn.ih [at] gmail.com Department of Higher Geodesy and Astronomy, Lviv Polytechnic National University
Lviv, Ukraine
Andrii Romanovskyi No androm1297 [at] gmail.com Department of Photogrammetry and Geoinformatiс, Lviv Polytechnic National University
Lviv, Ukraine
Nazarii Danyliv No konon.mobind [at] gmail.com Department of Engineering Geodesy, Lviv Polytechnic National University
Lviv, Ukraine

I and my co-authors (if any) authorize the use of the Paper in accordance with the Creative Commons CC BY license

First publshed on this website: 31.10.2018 - 17:58
Abstract

A network of triangles with vertices of GNSS observation points is created. The deformation parameters of each triangle were calculated using the software "GPS TriangleStrainCalculator" developed by UNAVCO. The obtained values are used to construct maps of distribution of velocities of dilation and displacement of points for the period of 2003-2018 years, that shows movements of tectonic plates in the area Penola Strait.

References

[1] O. Tereshhuk, “Suchasni suputnykovi tekhnolohii u doslidzhenni heodynamichnykh protsesiv,” [Modern satelite technologies in the research of geodynamic processes]. Heodeziia, kartohrafiia i aerofotoznimannia [Geodesy, Cartography and Aerial Photography], 2009, pp. 49–53.

[2] A.I. Kulchytskyi, “Poverkhneva ta hlybynna dynamika zemli za rezultatamy opratsiuvannia GNSS-vymiriv i heoloho-heofizychnykh danykh (metodolohichnyi aspekt),” [Surface and deep dynamics of the earth on the results of GNSS-measurement and geological and geophysical data prospects (methodological aspect)]. Heodynamika [Geodynamics], no. 1, 2012, pp. 54–57.

[3] K.R. Tretiak, F.K.F. Al-Alusi and L.V. Babii, “Doslidzennia vzaiemozviazku mizh zminamy ta pererozpodilom momentu impulsu zemli, antarktychnoi tektonichnoi plyty, atmosfery ta okeanu,” [Research interaction between changes and reverse moment impulse of the earth, antarctic tectonic plate, atmosphere and ocean]. Heodynamika [Geodynamics], no. 1, 2018, pp. 5-26.

[4] K.R. Tretiak and Y.I. Holubinka. “Otsinka ta dyferentsiatsiia rukhiv zemnoi kory antarktydy,” [Evaluation and diferentiation of earth crust Antarctica]. Ukrainskyi antarktychnyi zhurnal [Ukrainian Antarctic Magazine], no. 4, 2006, pp. 72-83.

[5] A.I. Kulchytskyi, K.R. Tretiak and Y.I. Holubinka. “Detalizovana heodynamichna model rozlomu Penola (antarktychnyi pivostriv) na osnovi heodezychnykh vymiriv ta heoloho-heofizychnykh danykh,” [Detailed geodynamic model of Penola fault (Antarctic Peninsula) on the basis of geodetic measurements and geological and geophysical data]. Heodynamika [Geodynamics], no. 1(9), 2010, pp. 5-9.

[6] A. Zanutta et al., “New Geodetic and Gravimetric Maps to Infer Geodynamics of Antarctica with Insights on Victoria Land,” Remote Sensing, no.10, 2018.

[7] A. Richter et al., “Observational evidence on the stability of the hydro-glaciological regime of subglacial Lake Vostok,” Geophysical Research Letters, 35. 10.1029/2008GL033397, 2008.

Official paper