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Title : The Waveform Inversion of Mainshock and Aftershock Data of the 2006 M6.3 Yogyakarta Earthquake
Author :

HIJRAH SAPUTRA (1) Dr. Wahyudi, M.S. (2) Iman Suardi (3) Ade Anggraini S.Si, M.T (4) Dr.rer.nat. Wiwit Suryanto, S.Si., M.Si. (5)

Date : 1 2020
Keyword : aftershock Yogyakarta earthquake,moment tensor,waveform modeling aftershock Yogyakarta earthquake,moment tensor,waveform modeling
Abstract : This research was examines the focal mechanism associated with the mainshock and three aftershocks of the magnitude 6.3 Yogyakarta earthquake on May 27, 2006. This study, therefore, aims to provide a cleareranswer on the source mechanism of the earthquake, which has been debated. Data were obtained from the mainshock and aftershock sources, on June 8, 9, and 16, 2006. The mainshock and three aftershocks were used to conduct waveform inversion by calculating the Green's functions through the extended reflectivity method of the near-field and the far-field signal component. The mainshock's focal mechanism has a strike, dip, and range angle of 243.40o, 77.50o, and -28.30o, respectively. Furthermore, the mainshock is not a pure strike-slip as previously hypothesized. The focal mechanism for the aftershock earthquake source on Mw 4.4, obtained on June 8, had a strike, dip, rake, and variance of 192.20o, 29.70o, -48.30o and 0.22, respectively. This aftershock had a different segment from the mainshock event and those obtained on the 9 and 16 of June with the same type of faulting as the mainshock with variance values of 0.195 and 0.243. These results showed that the mainshock of May 27, 2006, activated the aftershock on June 8, with a different type of fault.
Group of Knowledge : Geofisika
Original Language : English
Level : Internasional
Status :
Published
Document
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1 Confirmation of your submission Geoscience Letters - GOSL-D-20-00022 - ws@ugm_ac_id - Universitas Ga.pdf
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2 s40562-021-00176-w.pdf
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3 The waveform inversion of mainshock and aftershock data of the 2006 M6_3 Yogyakarta earthquake-compressed.pdf
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