2007/10/24 21:02:51 -3.91 101.06 30
The following compares this source inversion to the USGS Rapid Moment Tensor Solution and to the Harvard CMT solutions, if they are available.
The following broadband stations passed the QC and were used for the source inversion. AAK ADK AFI AML ANTO ARU BFO BFZ BILL BJT BKZ BRVK CAN CASY CEL CHM CTAO CUC DPC EIL EKS2 ENH ERM FUNA FURI GNI GRFO GUMO HIA HIZ HNR IDI INCN KBK KBS KEV KHZ KIEV KIV KMBO KMNB KONO KURK KZA LSA LSZ LVZ MAJO MBAR MDJ MIDW MSEY NACB NWAO OBN ODZ OUZ PAF PATS PET PMG QRZ QSPA RAO RER RPZ SBA SNAA SNZO SSLB SUR SUW TARA TATO TAU TIP TIR TIRR TIXI TKM2 TLY TPUB TSUM TUE TWGB UCH ULHL ULN URZ USP VLC VSL VSU WDD WPVZ WRAB YAK YHNB YSS
All observed and Greens function waveforms are corrected to instrument response to ground velocity in meters/sec for the passband of 0.004 - 5 Hz. The traces were then lowpass filtered at 0.25 Hz and interpolated to a sample rate of 1 second.
The moment tensor solution used has the parameters:
HS=20.0 STK=322 DIP=13 RAKE=108 MW=6.8 The Green's function closest to the desired depth was DEP=0200 , where (DEP/10) is the computed depth.The cut windows attempt to include the P, pP, sP, pS, S and sS arrivals. However, one must be very careful about the fact that PP may be included in some distance ranges.
The waveforms are then bandpass filtered by the application of the following high- and low-pass stages (an optional microseism filter):
hp c 0.0083 2 lp c 0.0250 2 int br c 0.12 0.25 n 4 p 2The traces were next integrated to ground displacment in meters. Finally the observed data are interpolated to have the same sampling at the Green's functions.
The following filter ranges are used according to the moment magnitude Mw:
FILTER_BAND 1/FH(s) 1/FL(s) 1 60 12 Mw < 6.4 2 100 20 6.4 < Mw <= 6.9 3 120 40 Mw > 6.9
The map displays the distribution of stations used for this source inversion.
![]() Location of the earthquake (yellow star) and great circle path from the epicenter to each station (red) [created using GMT (Wessel, P., and W. H. F. Smith, New version of Generic Mapping Tools released, EOS Trans. AGU, 76 329, 1995.)] |
P-wave Z component |
![]() |
Observed (red) and predicted seismograms (blue) ordered by increasing epicentral distance. Each pair of traces is annotated with the wave type and a station identifier (station, network, and channel id's), epicentral distance in degrees, source-to-station azimuth in degrees. Each seismogram pair is plotted with the same scale and the peak amplitudes in meters are shown above to the left of each trace. The optimal time shift between the observed first arrival and the predicted first arrival (in seconds) is shown above the prediction on the right. Red circles flag seismograms with amplitude misfits of a factor of 2 or more. |
SH-wave T component |
![]() |
Observed (red) and predicted seismograms (blue) ordered by increasing epicentral distance. Each pair of traces is annotated with the wave type and a station identifier (station, network, and channel id's), epicentral distance in degrees, source-to-station azimuth in degrees. Each seismogram pair is plotted with the same scale and the peak amplitudes in meters are shown above to the left of each trace. The optimal time shift between the observed first arrival and the predicted first arrival (in seconds) is shown above the prediction on the right. Red circles flag seismograms with amplitude misfits of a factor of 2 or more. |
SV-wave R component |
![]() |
Observed (red) and predicted seismograms (blue) ordered by increasing epicentral distance. Each pair of traces is annotated with the wave type and a station identifier (station, network, and channel id's), epicentral distance in degrees, source-to-station azimuth in degrees. Each seismogram pair is plotted with the same scale and the peak amplitudes in meters are shown above to the left of each trace. The optimal time shift between the observed first arrival and the predicted first arrival (in seconds) is shown above the prediction on the right. Red circles flag seismograms with amplitude misfits of a factor of 2 or more. |
AAKKNLHR AAKKNLHT AAKKNLHZ ADKIU00LHR ADKIU00LHT ADKIU00LHZ AFIIU00LHR AFIIU00LHT AFIIU00LHZ AFIIU10LHR AFIIU10LHT AFIIU10LHZ AMLKNLHR AMLKNLHT AMLKNLHZ ANTOIU00LHR ANTOIU00LHT ANTOIU00LHZ ARUII00LHR ARUII00LHT ARUII00LHZ BFOII00LHR BFOII00LHT BFOII00LHZ BFZNZ10LHR BFZNZ10LHT BFZNZ10LHZ BILLIU00LHR BILLIU00LHT BILLIU00LHZ BJTIC00LHR BJTIC00LHT BJTIC00LHZ BKZNZ10LHR BKZNZ10LHT BKZNZ10LHZ BRVKII00LHR BRVKII00LHT BRVKII00LHZ CANG00LHR CANG00LHT CANG00LHZ CASYIU00LHR CASYIU00LHT CASYIU00LHZ CASYIU10LHR CASYIU10LHT CASYIU10LHZ CELMNLHR CELMNLHT CELMNLHZ CHMKNLHR CHMKNLHT CHMKNLHZ CTAOIU00LHR CTAOIU00LHT CTAOIU00LHZ CUCMNLHR CUCMNLHT CUCMNLHZ DPCCZLHR DPCCZLHT DPCCZLHZ EILGELHR EILGELHT EILGELHZ EKS2KNLHR EKS2KNLHT EKS2KNLHZ ENHIC00LHR ENHIC00LHT ENHIC00LHZ ENHIC10LHR ENHIC10LHT ENHIC10LHZ ERMII00LHR ERMII00LHT ERMII00LHZ FUNAIU00LHZ FUNAIU10LHR FUNAIU10LHT FUNAIU10LHZ FURIIU00LHR FURIIU00LHT FURIIU00LHZ FURIIU10LHR FURIIU10LHT FURIIU10LHZ GNIIU00LHR GNIIU00LHT GNIIU00LHZ GRFOIULHR GRFOIULHT GRFOIULHZ GUMOIU00LHR GUMOIU00LHT GUMOIU00LHZ GUMOIU10LHR GUMOIU10LHT GUMOIU10LHZ HIAIC00LHR HIAIC00LHT HIAIC00LHZ HIZNZ10LHR HIZNZ10LHT HIZNZ10LHZ HNRIU00LHR HNRIU00LHT HNRIU00LHZ HNRIU10LHR HNRIU10LHT HNRIU10LHZ IDIMNLHR IDIMNLHT IDIMNLHZ INCNIU00LHR INCNIU00LHT INCNIU00LHZ INCNIU10LHR INCNIU10LHT INCNIU10LHZ KBKKNLHR KBKKNLHT KBKKNLHZ KBSIU00LHR KBSIU00LHT KBSIU00LHZ KBSIU10LHR KBSIU10LHT KBSIU10LHZ KEVIU00LHR KEVIU00LHT KEVIU00LHZ KEVIU10LHR KEVIU10LHT KEVIU10LHZ KHZNZ10LHR KHZNZ10LHT KHZNZ10LHZ KIEVIU00LHR KIEVIU00LHT KIEVIU00LHZ KIVII00LHR KIVII00LHT KIVII00LHZ KMBOIU00LHR KMBOIU00LHT KMBOIU00LHZ KMBOIU10LHR KMBOIU10LHT KMBOIU10LHZ KMNBTWLHR KMNBTWLHT KMNBTWLHZ KONOIU00LHR KONOIU00LHT KONOIU00LHZ KONOIU10LHR KONOIU10LHT KONOIU10LHZ KURKII00LHR KURKII00LHT KURKII00LHZ KZAKNLHR KZAKNLHT KZAKNLHZ LSAIC00LHR LSAIC00LHT LSAIC00LHZ LSAIC10LHR LSAIC10LHT LSAIC10LHZ LSZIU00LHR LSZIU00LHT LSZIU00LHZ LSZIU10LHR LSZIU10LHT LSZIU10LHZ LVZII00LHR LVZII00LHT LVZII00LHZ MAJOIU00LHR MAJOIU00LHT MAJOIU00LHZ MAJOIU10LHR MAJOIU10LHT MAJOIU10LHZ MBARII00LHR MBARII00LHT MBARII00LHZ MDJIC00LHR MDJIC00LHT MDJIC00LHZ MDJIC10LHR MDJIC10LHT MDJIC10LHZ MIDWIU00LHR MIDWIU00LHT MIDWIU00LHZ MSEYII00LHR MSEYII00LHT MSEYII00LHZ NACBTWLHR NACBTWLHT NACBTWLHZ NACBTWLLZ NWAOIU00LHR NWAOIU00LHT NWAOIU00LHZ OBNII00LHR OBNII00LHT OBNII00LHZ ODZNZ10LHR ODZNZ10LHT ODZNZ10LHZ OUZNZ10LHR OUZNZ10LHT OUZNZ10LHZ PAFG10LHR PAFG10LHT PAFG10LHZ PATSPSLHR PATSPSLHT PATSPSLHZ PETIU00LHR PETIU00LHT PETIU00LHZ PMGIU00LHR PMGIU00LHT PMGIU00LHZ PMGIU10LHR PMGIU10LHT PMGIU10LHZ QRZNZ10LHR QRZNZ10LHT QRZNZ10LHZ QSPAIU00LHR QSPAIU00LHT QSPAIU00LHZ QSPAIU10LHR QSPAIU10LHT QSPAIU10LHZ QSPAIU20LHR QSPAIU20LHT QSPAIU20LHZ QSPAIU30LHZ QSPAIU50LHR QSPAIU50LHT QSPAIU50LHZ RAOIU00LHZ RAOIU10LHR RAOIU10LHT RAOIU10LHZ RERG00LHR RERG00LHT RERG00LHZ RPZNZ10LHR RPZNZ10LHT RPZNZ10LHZ SBAIU00LHR SBAIU00LHT SBAIU00LHZ SNAAGELHR SNAAGELHT SNAAGELHZ SNZOIU00LHR SNZOIU00LHT SNZOIU00LHZ SNZOIU10LHR SNZOIU10LHT SNZOIU10LHZ SSLBTWLHR SSLBTWLHT SSLBTWLHZ SSLBTWLLZ SURII00LHR SURII00LHT SURII00LHZ SUWGELHR SUWGELHT SUWGELHZ TARAIU00LHZ TARAIU10LHR TARAIU10LHT TARAIU10LHZ TATOIU00LHR TATOIU00LHT TATOIU00LHZ TATOIU10LHR TATOIU10LHT TATOIU10LHZ TAUII00LHR TAUII00LHT TAUII00LHZ TIPMNLHR TIPMNLHT TIPMNLHZ TIRMNLHR TIRMNLHT TIRMNLHZ TIRRGELHR TIRRGELHT TIRRGELHZ TIXIIU00LHR TIXIIU00LHT TIXIIU00LHZ TKM2KNLHR TKM2KNLHT TKM2KNLHZ TLYII00LHR TLYII00LHT TLYII00LHZ TPUBTWLHR TPUBTWLHT TPUBTWLHZ TPUBTWLLZ TSUMIU00LHR TSUMIU00LHT TSUMIU00LHZ TSUMIU10LHR TSUMIU10LHT TSUMIU10LHZ TUEMNLHR TUEMNLHT TUEMNLHZ TWGBTWLHR TWGBTWLHT TWGBTWLHZ UCHKNLHR UCHKNLHT UCHKNLHZ ULHLKNLHR ULHLKNLHT ULHLKNLHZ ULNIU00LHR ULNIU00LHT ULNIU00LHZ URZNZ10LHR URZNZ10LHT URZNZ10LHZ USPKNLHR USPKNLHT USPKNLHZ VLCMNLHR VLCMNLHT VLCMNLHZ VSLMNLHR VSLMNLHT VSLMNLHZ VSUGELHR VSUGELHT VSUGELHZ WDDMNLHR WDDMNLHT WDDMNLHZ WPVZNZ10LHR WPVZNZ10LHT WPVZNZ10LHZ WRABII00LHR WRABII00LHT WRABII00LHZ WRABII10LHR WRABII10LHT WRABII10LHZ YAKIU00LHR YAKIU00LHT YAKIU00LHZ YHNBTWLHR YHNBTWLHT YHNBTWLHZ YSSIU00LHR YSSIU00LHT YSSIU00LHZ
Starting Processing : Wed Nov 14 14:05:11 UTC 2007 Starting wget to get files : Wed Nov 14 14:05:24 UTC 2007 Unpacking SEED volume : Wed Nov 14 14:05:24 UTC 2007 Starting deconvolution : Wed Nov 14 14:05:28 UTC 2007 Starting trace rotation : Wed Nov 14 14:06:57 UTC 2007 Starting distance selection : Wed Nov 14 14:07:10 UTC 2007 Starting trace QC : Wed Nov 14 14:07:14 UTC 2007 Starting synthetic : Wed Nov 14 14:07:14 UTC 2007 Starting documentation : Wed Nov 14 14:09:00 UTC 2007 Processing Completion : Wed Nov 14 14:09:01 UTC 2007