The waveform inversion of mainshock and aftershock data of the 2006 M6.3 Yogyakarta earthquake

• Published in: Geoscience letters Vol. 8; no. 1; pp. 1 - 22
• Main Authors: Saputra, Hijrah, Wahyudi, Wahyudi, Suardi, Iman, Anggraini, Ade, Suryanto, Wiwit
• Format: Journal Article
• Language: English
• Published: Cham Springer International Publishing 13.03.2021; Springer Nature B.V; SpringerOpen
• Subjects: Aftershock; Aftershocks; Asperity; Atmospheric Sciences; Bandpass filters; Bayesian analysis; Biogeosciences; Distribution; Earth and Environmental Science; Earth Sciences; Earthquakes; Geophysics/Geodesy; Inversion; Mainshock; Mathematical models; Moment tensor; Near fields; Near-field; Oceanography; Parameters; Planetology; Probability theory; Reflectance; Research Letter; Seismic activity; Slip; Stress concentration; Stress distribution; Tectonics; Teleseismic; Tensors; Trial and error methods; Wave data; Waveforms; Aftershock; Near-field; Mainshock; Inversion; Teleseismic; Joint inversion; Moment tensor
• ISSN: 2196-4092; 2196-4092
• DOI: 10.1186/s40562-021-00176-w

This study comprehensively investigates the source mechanisms associated with the mainshock and aftershocks of the Mw = 6.3 Yogyakarta earthquake which occurred on May 27, 2006. The process involved using moment tensor inversion to determine the fault plane parameters and joint inversion which were further applied to understand the spatial and temporal slip distributions during the earthquake. Moreover, coseismal slip distribution was overlaid with the relocated aftershock distribution to determine the stress field variations around the tectonic area. Meanwhile, the moment tensor inversion made use of near-field data and its Green’s function was calculated using the extended reflectivity method while the joint inversion used near-field and teleseismic body wave data which were computed using the Kikuchi and Kanamori methods. These data were filtered through a trial-and-error method using a bandpass filter with frequency pairs and velocity models from several previous studies. Furthermore, the Akaike Bayesian Information Criterion (ABIC) method was applied to obtain more stable inversion results and different fault types were discovered. Strike–slip and dip-normal were recorded for the mainshock and similar types were recorded for the 8th aftershock while the 9th and 16th June were strike slips. However, the fault slip distribution from the joint inversion showed two asperities. The maximum slip was 0.78 m with the first asperity observed at 10 km south/north of the mainshock hypocenter. The source parameters discovered include total seismic moment M 0  = 0.4311E + 19 (Nm) or Mw = 6.4 with a depth of 12 km and a duration of 28 s. The slip distribution overlaid with the aftershock distribution showed the tendency of the aftershock to occur around the asperities zone while a normal oblique focus mechanism was found using the joint inversion.