The source parameters of the Çubukdağ (W. Turkey) earthquake of 1986 October 11

Tuncay Taymaz

doi:10.1111/j.1365-246X.1993.tb02545.x

The source parameters of the Çubukdağ (W. Turkey) earthquake of 1986 October 11

Tuncay Taymaz^*

^*Corresponding author for this work

Department of Geophysical Engineering

Research output: Contribution to journal › Article › peer-review

33 Citations (Scopus)

Abstract

Long period P and SH waveforms and first motion polarities of P waves were used to determine the source parameters of the Çubukdaǧ (in the eastern section of the Büyük Menderes graben) earthquake of 1986 October 11, the waveforms used in this event include the WWSSN, and the digitally recorded seismograms of the DWWSSN, SRO and ASRO networks. the minimum misfit solution obtained by the inversion of teleseismic body waveforms are better constrained that those of the previously published Harvard Centroid‐Moment Tensor solution, and are in good agreement with field observations and the local geometry of the graben.

Original language	English
Pages (from-to)	260-267
Number of pages	8
Journal	Geophysical Journal International
Volume	113
Issue number	1
DOIs	https://doi.org/10.1111/j.1365-246X.1993.tb02545.x
Publication status	Published - Apr 1993

Keywords

Büyük Menderes graben
faulting
W. Turkey.
waveform inversion
Çubukdaǧ

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10.1111/j.1365-246X.1993.tb02545.x

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abstract = "Long period P and SH waveforms and first motion polarities of P waves were used to determine the source parameters of the {\c C}ubukdaǧ (in the eastern section of the B{\"u}y{\"u}k Menderes graben) earthquake of 1986 October 11, the waveforms used in this event include the WWSSN, and the digitally recorded seismograms of the DWWSSN, SRO and ASRO networks. the minimum misfit solution obtained by the inversion of teleseismic body waveforms are better constrained that those of the previously published Harvard Centroid‐Moment Tensor solution, and are in good agreement with field observations and the local geometry of the graben.",

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AB - Long period P and SH waveforms and first motion polarities of P waves were used to determine the source parameters of the Çubukdaǧ (in the eastern section of the Büyük Menderes graben) earthquake of 1986 October 11, the waveforms used in this event include the WWSSN, and the digitally recorded seismograms of the DWWSSN, SRO and ASRO networks. the minimum misfit solution obtained by the inversion of teleseismic body waveforms are better constrained that those of the previously published Harvard Centroid‐Moment Tensor solution, and are in good agreement with field observations and the local geometry of the graben.

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The source parameters of the Çubukdağ (W. Turkey) earthquake of 1986 October 11

Abstract

Keywords

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