Location

Location ANSS

The ANSS event ID is pr2020020006 and the event page is at https://earthquake.usgs.gov/earthquakes/eventpage/pr2020020006/executive.

2020/01/20 09:56:21 17.971 -66.754 6.0 4.2 Puerto Rico

Focal Mechanism

USGS/SLU Moment Tensor Solution ENS 2020/01/20 09:56:21:0 17.97 -66.75 6.0 4.2 Puerto Rico Stations used: GS.PR01 GS.PR03 GS.PR05 IU.SJG PR.AGPR PR.AOPR PR.CELP PR.CRPR PR.ECPR PR.GCPR PR.OBIP PR.PRSN PR.UUPR Filtering commands used: cut o DIST/3.3 -40 o DIST/3.3 +50 rtr taper w 0.1 hp c 0.03 n 3 lp c 0.10 n 3 Best Fitting Double Couple Mo = 1.30e+22 dyne-cm Mw = 4.01 Z = 5 km Plane Strike Dip Rake NP1 57 63 -104 NP2 265 30 -65 Principal Axes: Axis Value Plunge Azimuth T 1.30e+22 17 157 N 0.00e+00 12 63 P -1.30e+22 69 299 Moment Tensor: (dyne-cm) Component Value Mxx 9.67e+21 Mxy -3.60e+21 Mxz -5.47e+21 Myy 5.56e+20 Myz 5.27e+21 Mzz -1.02e+22 ############## ###################### ############################ ##########------------######## #######----------------------##### #####---------------------------###- ####---------------------------------- ###---------------------------------##-- ##------------ -----------------#####- ##------------- P ----------------#######- #-------------- ---------------######### #------------------------------########### -----------------------------############# -------------------------############### -----------------------################# ------------------#################### -------------####################### ################################## ##################### ###### #################### T ##### ################# ## ############## Global CMT Convention Moment Tensor: R T P -1.02e+22 -5.47e+21 -5.27e+21 -5.47e+21 9.67e+21 3.60e+21 -5.27e+21 3.60e+21 5.56e+20 Details of the solution is found at http://www.eas.slu.edu/eqc/eqc_mt/MECH.NA/20200120095621/index.html

Preferred Solution

      STK = 265
      DIP = 30
     RAKE = -65
       MW = 4.01
       HS = 5.0

The NDK file is 20200120095621.ndk The waveform inversion is preferred.

Magnitudes

Given the availability of digital waveforms for determination of the moment tensor, this section documents the added processing leading to mLg, if appropriate to the region, and M_L by application of the respective IASPEI formulae. As a research study, the linear distance term of the IASPEI formula for M_L is adjusted to remove a linear distance trend in residuals to give a regionally defined M_L. The defined M_L uses horizontal component recordings, but the same procedure is applied to the vertical components since there may be some interest in vertical component ground motions. Residual plots versus distance may indicate interesting features of ground motion scaling in some distance ranges. A residual plot of the regionalized magnitude is given as a function of distance and azimuth, since data sets may transcend different wave propagation provinces.

ML Magnitude

Left: ML computed using the IASPEI formula for Horizontal components. Center: ML residuals computed using a modified IASPEI formula that accounts for path specific attenuation; the values used for the trimmed mean are indicated. The ML relation used for each figure is given at the bottom of each plot. Right: Residuals from new relation as a function of distance and azimuth.

Left: ML computed using the IASPEI formula for Vertical components (research). Center: ML residuals computed using a modified IASPEI formula that accounts for path specific attenuation; the values used for the trimmed mean are indicated. The ML relation used for each figure is given at the bottom of each plot. Right: Residuals from new relation as a function of distance and azimuth.

Context

Waveform Inversion using wvfgrd96

The focal mechanism was determined using broadband seismic waveforms. The location of the event (star) and the stations used for (red) the waveform inversion are shown in the next figure.

Location of broadband stations used for waveform inversion

The program wvfgrd96 was used with good traces observed at short distance to determine the focal mechanism, depth and seismic moment. This technique requires a high quality signal and well determined velocity model for the Green's functions. To the extent that these are the quality data, this type of mechanism should be preferred over the radiation pattern technique which requires the separate step of defining the pressure and tension quadrants and the correct strike.

The observed and predicted traces are filtered using the following gsac commands:

cut o DIST/3.3 -40 o DIST/3.3 +50
rtr
taper w 0.1
hp c 0.03 n 3 
lp c 0.10 n 3 

           DEPTH  STK   DIP  RAKE   MW    FIT
WVFGRD96    1.0   300    65     0   3.59 0.2874
WVFGRD96    2.0   290    35   -10   3.83 0.3927
WVFGRD96    3.0   280    30   -30   3.92 0.5802
WVFGRD96    4.0   275    30   -45   3.97 0.6825
WVFGRD96    5.0   265    30   -65   4.01 0.7207
WVFGRD96    6.0   265    30   -65   4.01 0.7132
WVFGRD96    7.0   255    30   -80   4.03 0.6830
WVFGRD96    8.0   260    30   -75   4.11 0.6749
WVFGRD96    9.0   260    30   -75   4.10 0.6221
WVFGRD96   10.0   265    30   -65   4.08 0.5695
WVFGRD96   11.0   290    55     5   4.01 0.5335
WVFGRD96   12.0   290    55     5   4.02 0.5096
WVFGRD96   13.0   290    60    15   4.04 0.4906
WVFGRD96   14.0   290    60    20   4.05 0.4751
WVFGRD96   15.0   295    55    15   4.06 0.4632
WVFGRD96   16.0   300    55    15   4.08 0.4564
WVFGRD96   17.0   300    55    15   4.09 0.4519
WVFGRD96   18.0   300    55    20   4.10 0.4479
WVFGRD96   19.0   300    55    20   4.11 0.4459
WVFGRD96   20.0   300    55    20   4.12 0.4446
WVFGRD96   21.0   300    55    20   4.13 0.4423
WVFGRD96   22.0   305    55    25   4.14 0.4416
WVFGRD96   23.0   305    55    30   4.15 0.4442
WVFGRD96   24.0   305    55    30   4.16 0.4471
WVFGRD96   25.0   305    55    30   4.16 0.4517
WVFGRD96   26.0   305    55    30   4.17 0.4544
WVFGRD96   27.0   305    55    30   4.18 0.4575
WVFGRD96   28.0   305    55    35   4.18 0.4591
WVFGRD96   29.0   305    55    35   4.19 0.4617

The best solution is

WVFGRD96    5.0   265    30   -65   4.01 0.7207

The mechanism corresponding to the best fit is

Figure 1. Waveform inversion focal mechanism

The best fit as a function of depth is given in the following figure:

Figure 2. Depth sensitivity for waveform mechanism

The comparison of the observed and predicted waveforms is given in the next figure. The red traces are the observed and the blue are the predicted. Each observed-predicted component is plotted to the same scale and peak amplitudes are indicated by the numbers to the left of each trace. A pair of numbers is given in black at the right of each predicted traces. The upper number it the time shift required for maximum correlation between the observed and predicted traces. This time shift is required because the synthetics are not computed at exactly the same distance as the observed, the velocity model used in the predictions may not be perfect and the epicentral parameters may be be off. A positive time shift indicates that the prediction is too fast and should be delayed to match the observed trace (shift to the right in this figure). A negative value indicates that the prediction is too slow. The lower number gives the percentage of variance reduction to characterize the individual goodness of fit (100% indicates a perfect fit).

The bandpass filter used in the processing and for the display was

cut o DIST/3.3 -40 o DIST/3.3 +50
rtr
taper w 0.1
hp c 0.03 n 3 
lp c 0.10 n 3 

Figure 3. Waveform comparison for selected depth. Red: observed; Blue - predicted. The time shift with respect to the model prediction is indicated. The percent of fit is also indicated. The time scale is relative to the first trace sample.

Focal mechanism sensitivity at the preferred depth. The red color indicates a very good fit to the waveforms. Each solution is plotted as a vector at a given value of strike and dip with the angle of the vector representing the rake angle, measured, with respect to the upward vertical (N) in the figure.

A check on the assumed source location is possible by looking at the time shifts between the observed and predicted traces. The time shifts for waveform matching arise for several reasons:

• The origin time and epicentral distance are incorrect
• The velocity model used for the inversion is incorrect
• The velocity model used to define the P-arrival time is not the same as the velocity model used for the waveform inversion (assuming that the initial trace alignment is based on the P arrival time)

 Time_shift = A + B cos Azimuth + C Sin Azimuth

The time shifts for this inversion lead to the next figure:

The derived shift in origin time and epicentral coordinates are given at the bottom of the figure.

Velocity Model

The WUS.model used for the waveform synthetic seismograms and for the surface wave eigenfunctions and dispersion is as follows (The format is in the model96 format of Computer Programs in Seismology).

MODEL.01
Model after     8 iterations
ISOTROPIC
KGS
FLAT EARTH
1-D
CONSTANT VELOCITY
LINE08
LINE09
LINE10
LINE11
      H(KM)   VP(KM/S)   VS(KM/S) RHO(GM/CC)         QP         QS       ETAP       ETAS      FREFP      FREFS
     1.9000     3.4065     2.0089     2.2150  0.302E-02  0.679E-02   0.00       0.00       1.00       1.00    
     6.1000     5.5445     3.2953     2.6089  0.349E-02  0.784E-02   0.00       0.00       1.00       1.00    
    13.0000     6.2708     3.7396     2.7812  0.212E-02  0.476E-02   0.00       0.00       1.00       1.00    
    19.0000     6.4075     3.7680     2.8223  0.111E-02  0.249E-02   0.00       0.00       1.00       1.00    
     0.0000     7.9000     4.6200     3.2760  0.164E-10  0.370E-10   0.00       0.00       1.00       1.00