Atıf İçin Kopyala
Pırtı A., Kurtulgu Z., Eren M.
GEODESY AND CARTOGRAPHY, cilt.50, sa.4, ss.156-161, 2024 (Scopus)
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Yayın Türü:
Makale / Tam Makale
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Cilt numarası:
50
Sayı:
4
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Basım Tarihi:
2024
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Doi Numarası:
10.3846/gac.2024.20007
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Dergi Adı:
GEODESY AND CARTOGRAPHY
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Derginin Tarandığı İndeksler:
Scopus, Academic Search Premier, Aerospace Database, Central & Eastern European Academic Source (CEEAS), Geobase, Directory of Open Access Journals, Civil Engineering Abstracts
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Sayfa Sayıları:
ss.156-161
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Yıldız Teknik Üniversitesi Adresli:
Evet
Özet
ad, and 90 more aftershocks followed. These earthquakes, which were felt across the area,
enter began. In its first assessment, the United States Geological Sur-
vey gave the earthquake a magnitude of 6.3 at a depth of 16 kilometers. In this study, firstly, GNSS data
belonging to ARST station in 30
seconds recording interval were downloaded into CSRS-PPP. GNSS data
was processed as static and then was processed as epoch to epoch by using kinematic method. The coor
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dinate differences between the obtained coordinates by using the kinematic processing and the obtained
coordinates by using the static processing were computed. According to the obtained results, a horizontal
movement of approximately 8.30
cm in the south-west direction was observed at the ARST station, which is
the closest to the earthquake center. magnitude of 6.3 at a depth of 16 kilometers. In this study, firstly, GNSS data
belonging to ARST station in 30
seconds recording interval were downloaded into CSRS-PPP. GNSS data
was processed as static and then was processed as epoch to epoch by using kinematic method. The coor
-
dinate differences between the obtained coordinates by using the kinematic processing and the obtained
coordinates by using the static processing were computed. According to the obtained results, a horizontal
movement of approximately 8.30
cm in the south-west direction was observed at the ARST station, which is
the closest to the earthquake center.