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Published on: August 7, 2017
On the rotation of teleseismic seismograms based on the receiver function technique
M Wilde-Piórko1, M Grycuk1, M Polkowski1
1Faculty of Physics, University of Warsaw, Pasteura 5, 02-093 Warszawa, Poland.
This study introduces an improved automatic method for analyzing seismic receiver functions (RFs), enhancing the accuracy of determining seismic wave properties. The new procedure is effective even with complex geological structures and potential instrument orientation errors.
Area of Science:
- Geophysics
- Seismology
- Earth Sciences
Background:
- The receiver function (RF) technique is crucial for studying Earth's crust and upper mantle using seismic data.
- Accurate determination of seismic event back azimuth and polarization is essential for reliable RF analysis.
Purpose of the Study:
- To develop and validate a modified automatic procedure for calculating back azimuth and polarization angles from seismic receiver functions.
- To assess the robustness of the new procedure against seismic station location and potential instrument misorientation.
Main Methods:
- A modified automatic procedure was developed to determine back azimuth and polarization angles from teleseismic event seismograms.
- The method was tested using data from six seismic stations in Poland (3 permanent, 3 temporary).
- Rayleigh wave polarization analysis and synthetic modeling of RFs for 2.5D crustal models were employed.
Main Results:
- The proposed method accurately determines back azimuth and polarization angles for teleseismic events.
- The procedure demonstrated robustness against incorrect seismometer orientation, confirmed by Rayleigh wave analysis.
- Synthetic modeling confirmed the method's effectiveness in complex geological settings with dipping layers up to 60 km depth.
Conclusions:
- The modified automatic procedure offers a reliable and robust approach for seismic receiver function analysis.
- This technique improves the investigation of crustal and upper mantle structures, even in geologically complex regions.
- The method's insensitivity to orientation errors enhances its applicability in real-world seismic network operations.
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