[IGSSTATION-8756] Possible co-seismic displacements: CKSV, KMNM, NCKU, TCMS, TNML, TWTF

igs-rf at ign.fr igs-rf at ign.fr
Thu Apr 4 07:44:55 UTC 2024


# Author : Paul Rebischung
# Contact : igs-rf at ign.fr
# Subject : Possible co-seismic displacements: CKSV, KMNM, NCKU, TCMS, TNML, TWTF
# 
# This is a notification that recent earthquake(s) may have induced noticeable displacements of one or more IGS stations.
#
# This message and the table below were generated automatically based on the following procedure:
# * The Global Centroid-Moment-Tensor (CMT) catalog (https://www.globalcmt.org/) is scanned every day for new earthquakes.
# * For every new earthquake, the width, length and slip of the rupture are estimated from:
#    - Yen & Ma (2012; https://doi.org/10.1785/0120100046)'s scaling law if the earthquake magnitude is less than 7.6;
#    - Mai & Beroza (2000; https://doi.org/10.1785/0119990126)'s scaling law it the earthquake magnitude is larger.
#    (See justification for these choices in Métivier et al., 2014; https://doi.org/10.1002/2014JB011280.)
# * For every new earthquake, based on its estimated CMT and rupture parameters, co-seismic displacements are calculated
#   at all IGS stations using Okada (1985; https://doi.org/10.1785/BSSA0750041135)'s approach. Given that the CMT inversion
#   from seismic waves gives rise to two possible solutions for the rupture plane, two possible co-seismic displacements
#   are calculated for every station and earthquake.
# * If any calculated 3D co-seismic displacement of an IGS station exceeds 1 mm, it is included in the table below.
#
# Warning : The co-seismic displacements thus calculated rely on several coarse approximations. They should not be used as
#           estimates of the actual co-seismic displacements, but only as rough orders of magnitude.
# 
# The column "RF?" in the table below indicates whether each station is part of the current IGS reference frame (IGS20),
# hence might need to stop being used as a reference frame station after the earthquake.
# 
# The successive co-seismic displacements thus calculated are compiled in a cumulative table available at:
# ftp://igs-rf.ign.fr/pub/coseismic/IGS_coseismic.dat
# 
#__________station_________   ___________________________earthquake_____________________________   dist_   _____displacement1_____   _____displacement2_____
#sta_ lon[deg] lat[deg] RF?   date_______________ Mw_ location________________ lon[deg] lat[deg]   d[km]   dE[mm]_ dN[mm]_ dH[mm]_   dE[mm]_ dN[mm]_ dH[mm]_
#-----------------------------------------------------------------------------------------------------------------------------------------------------------
 CKSV  120.220   22.999 Yes   2024-04-02 23:58:11 7.4 Taiwan                    121.560   23.820     164       6.1    -0.2    -4.1       5.7    -0.3    -4.8
 KMNM  118.389   24.464 Yes   2024-04-02 23:58:11 7.4 Taiwan                    121.560   23.820     330       7.3    -2.6     0.2       7.2    -2.6     0.3
 NCKU  120.223   22.997 No    2024-04-02 23:58:11 7.4 Taiwan                    121.560   23.820     164       6.1    -0.2    -4.1       5.6    -0.3    -4.8
 TCMS  120.987   24.798 Yes   2024-04-02 23:58:11 7.4 Taiwan                    121.560   23.820     123      21.5   -27.7    -6.2      23.8   -31.1    -5.4
 TNML  120.987   24.798 Yes   2024-04-02 23:58:11 7.4 Taiwan                    121.560   23.820     123      21.5   -27.7    -6.2      23.8   -31.1    -5.4
 TWTF  121.164   24.954 No    2024-04-02 23:58:11 7.4 Taiwan                    121.560   23.820     132      12.3   -17.6    -3.7      13.4   -20.4    -4.4
 TCMS  120.987   24.798 Yes   2024-04-03 00:11:25 6.5 Taiwan                    121.670   24.060     107       1.8    -2.5     0.2       1.7    -2.4     0.2
 TNML  120.987   24.798 Yes   2024-04-03 00:11:25 6.5 Taiwan                    121.670   24.060     107       1.8    -2.5     0.2       1.7    -2.4     0.2
 TWTF  121.164   24.954 No    2024-04-03 00:11:25 6.5 Taiwan                    121.670   24.060     112       1.3    -2.5     0.2       1.3    -2.5     0.2


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