2004年至2020年Pienin-Klippen带的地球动力学研究

IF 0.7 Q4 ASTRONOMY & ASTROPHYSICS
Dominika Staniszewska, T. Liwosz, A. Pachuta, D. Próchniewicz, R. Szpunar
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引用次数: 0

摘要

摘要Pieniny地动力学试验场位于喀尔巴阡山脉内外部之间的中部。过去在Pienin-Klippen带(PKB)地区进行的地质动力学研究表明了新构造活动。调查的目的是确定附近的Podhale Flysh(FP)和Magura Nappe(MN)结构是否受到PKB新构造活动的影响。该研究的目的是确定位于Pieniny地质动力试验场3个主要结构附近的台站的运动速度和方向。12个GNSS站,包括6个位于PKB、3个位于MN和3个位于FP,组成了Pieniny地球动力学测试场。位于塔特拉山脉(TM)的三个全球导航卫星系统站点完成了整个地球动力学试验场。对2004年至2020年期间(由于缺乏观测,不包括2005年)进行的卫星观测进行了调查,以确定水平运动。使用IGb14参考系统,计算了该站的位置和速度。首先,使用每日会话来处理给定年份中平均观测时期的点的水平坐标。在长期解决方案中包括16个测量时期。基于南北和东西方向的水平速度残差,计算了该站的运动。将收集到的结果与欧洲导航卫星系统永久网络(EUREF)的信息以及先前关于北大西洋构造活动的研究结果进行了比较。本文给出并分析了利用GNSS测量PKB和附近结构(MN和FP)区域的水平位移计算结果。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geodynamic Studies in the Pieniny Klippen Belt in 2004–2020
ABSTRACT The Pieniny Geodynamic Test Field is situated in the middle of the region between the Inner and Outer Carpathians. Geodynamic research conducted in the past in the Pieniny Klippen Belt (PKB) region were suggestive of neotectonic activity. The goal of the investigation was to determine whether the nearby structures, the Podhale Flysh (FP) and the Magura Nappe (MN), are affected by neotectonic activity in the PKB. The goal of the study was to ascertain the velocity and direction of motion of stations situated close to the Pieniny Geodynamic Test Field’s 3 main structures. Twelve GNSS stations, including 6 in the PKB, 3 in the MN, and 3 in the FP, make up the Pieniny Geodynamic Test Field. Three GNSS sites in the Tatra Mountains (TM) complete the entire geodynamic test field. The satellite observations made between 2004 and 2020 (excluding the year 2005 due to lack of observation) were investigated to identify the horizontal movements. Using the IGb14 reference system, the station’s positions and velocities were calculated. First, daily sessions were used to process the horizontal coordinates of the points for an average observation epoch in a given year. Sixteen measurement epochs were included in the long-time solution. Based on the horizontal velocity residues in the north–south and east–west directions, the station’s movement was calculated. The collected results were compared to information from the EUREF Permanent GNSS Network (EUREF) and to the findings of prior research on the tectonic activity of the PKB. The results of horizontal displacements calculated using GNSS measurements in the area of the PKB and nearby structures—the MN and the FP are presented and analyzed in this article.
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CiteScore
1.00
自引率
11.10%
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