Seismometer Orientation Correction via Teleseismic Receiver Function Measurements in West Africa and Adjacent Islands

Author:

Osotuyi Abayomi Gaius12ORCID,Ni Sidao3ORCID,Chong Jiajun3ORCID,Jun Xie3ORCID,Akpan Ofonime4ORCID

Affiliation:

1. 1School of Earth and Space Sciences, University of Science and Technology of China, Hefei, China

2. 2Earthquake and Space Weather Laboratory, Geology Department, Obafemi Awolowo University, Ile–Ife, Nigeria

3. 3State Key Laboratory of Geodesy and Earth’s Dynamics, Innovation Academy for Precision Measurement Science and Technology, CAS, Wuhan, China

4. 4Centre for Geodesy and Geodynamics, Toro, Bauchi State, Nigeria

Abstract

AbstractTo establish a robust method of determining and correcting the misorientation of seismometers with radial and tangential components of the teleseismic receiver function (RF), we assess the measurement of the amplitude of P-wave phase arrivals at zero seconds (PRFamp method) and the energy of the width of the time window around the P-wave phase arrival (PRFenergy method) using varying Gaussian factors, ranging from 0.5 to 5.0 with equivalent cutoff frequencies. To understand the efficacy and discrepancies in these methods, and their results across different geological terrains, we conduct an assessment of their performance on 26 permanent seismic stations located in West Africa and adjacent islands. We conduct several tests to examine the effect of varying Gaussian factors on the estimates of misorientation. These effects are more noticeable in results from stations for which RFs are indicative of 3D or complex structures and islandic stations. Statistical analyses reveal good correlation between the results obtained from both the methods, although results from PRFamp method proves to be more stable due to their proximity to the statistical mean and standard deviation results. In comparison with the PRFenergy results, there is a smaller error difference and uncertainty, a higher correlation coefficient, a relatively lower standard deviation, and better convergence around the mean misorientation obtained using PRFamp. From both the methods, estimates from continental stations reveal similar trends, results from coastal stations tend to be consistent, whereas some island stations show a reverse trend in sensor misorientation classification. We propose that the PRFamp yields more consistent results and is less sensitive to subsurface heterogeneities. Gaussian filtering with an alpha value (α) of 1.5 is recommended as a trade-off between oversimplification and complications due to subsurface structures. However, we suggest that multiple approaches be adopted to provide robust bases for the estimation and comparison of sensor orientation correction calculations.

Publisher

Seismological Society of America (SSA)

Subject

Geophysics

Reference53 articles.

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