Rapid Moment Tensors (source mechanisms)
Distributed via E-mail
There are three groups who routinely produce moment tensors (source
mechanisms) shortly after large earthquakes which occur anywhere in
the world. These moment tensors are then distributed via e-mail. The three
groups are the NEIC, Harvard University, and the Earthquake Research
Institute in Tokyo. I include below an example from each. To subscribe or
learn more about each of these services, here are the e-mail addresses:
NEIC:
sedas@gldfs.cr.usgs.gov
Harvard University:
eq@geophysics.harvard.edu
ERI:
staff@center-sun.eri.u-tokyo.ac.jp
Note that there are other groups who routinely produce moment tensors
after earthquakes, but most of these groups focus on specific geographic
regions. The WWW site:
http://www.geophys.washington.edu/seismosurfing.html
is a good starting point for locating various groups which provide
electronic publication of earthquake information.
Here is a typical mailing from Harvard
--
From eq@seismology.harvard.edu Wed Nov 22 09:21:48 1995
Date: Wed, 22 Nov 95 09:56:55 EST
From: eq@seismology.harvard.edu (Seismoware)
To: cmtcustomers@seismology.harvard.edu
Subject: quick CMT
Content-Length: 1305
Here is the solution for the recent
event:
Nov 22, 1995; EGYPT ; Mw = 7.2
Misha Salganik
CENTROID, MOMENT TENSOR SOLUTION
HARVARD EVENT-FILE NAME M112295X
DATA USED: GSN
MANTLE WAVES: 37S, 95C, T=135
CENTROID LOCATION:
ORIGIN TIME 4:15:23.7 0.2
LAT 29.02N 0.01;LON 34.76E 0.01
DEP 15.0 FIX;HALF-DURATION 9.5
MOMENT TENSOR; SCALE 10**26 D-CM
MRR=-1.08 0.04; MTT=-2.87 0.04
MFF= 3.95 0.04; MRT= 4.57 0.42
MRF=-3.68 0.49; MTF=-3.96 0.03
PRINCIPAL AXES:
1.(T) VAL= 8.73;PLG=29;AZM= 59
2.(N) -2.03; 40; 301
3.(P) -6.71; 36; 173
BEST DOUBLE COUPLE:M0=7.7*10**26
NP1:STRIKE=203;DIP=40;SLIP= -6
NP2: 298; 86; -130
-----------
----------#########
---------##############
---------##################
--------############### ###
####----################ T ####
#######-################ ####
#######------####################
######-----------################
######--------------#############
######-----------------##########
#####--------------------######
#####-----------------------###
####---------- ------------
####--------- P -----------
###-------- ---------
##-----------------
-----------
----- End Included Message -----
Here is a typical mailing from ERI--
From staff@center-sun.eri.u-tokyo.ac.jp Wed Nov 22 01:59:55 1995
Date: Wed, 22 Nov 95 17:36:43 JST
From: staff@center-sun.eri.u-tokyo.ac.jp (staff)
To: auto-serve@center-sun.eri.u-tokyo.ac.jp
Subject: ERI AUTOCMT 11/22 EGYPT (ms 7.2)
Content-Length: 2641
* * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * *
* Following is a CMT solution automatically determined using a method very *
* similar to that developed by the Harvard group. *
* The solution is not checked by anyone at ERI and when the variance *
* reduction is below 10% or the station coverage is bad, it is often *
* unreliable. *
* *
* If you have any question or complaint, please contact to *
* hitosi@eri.u-tokyo.ac.jp *
* Hitoshi Kawakatsu *
* Earthquake Research Institute *
* * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * *
------------------------- ERI automatic CMT inversion -------------------------
EGYPT (ms 7.2)
1995-11-22 04:15:11.5 (QED) Mo=4.10**26(dyne-cm) Mw=7.0
lat: 28.50 lon: 34.70 dep: 10.0 (QED)
Data: bodywave [10,12,20,22mHz] ------------
coverage: 0- 60- 120- 180- 240- 300- --------------######
z-comp: 0 3 1 2 1 2 ----------------##########
r-comp: 0 3 1 2 1 2 -----------------############
t-comp: 0 3 1 2 1 2 -----------------############# T
Variance Reduction 22.3% of 27 records ####-------------##############
CMT solution: unit in 1e+26 (dyne-cm) #############----###################
lat: 28.54 lon: 34.68 dep: 33.2 (CMT) ################---#################
Mrr: -0.77 +- 0.11 Mrt: 0.54 +- 0.15 ################---------###########
Mtt: -2.20 +- 0.12 Mrf: 0.15 +- 0.20 ###############---------------######
Mff: 2.97 +- 0.19 Mtf: -3.12 +- 0.23 #############--------------------#
T-axis Val= 4.44 Plg= 1.1 Azm = 64.7 ############--------------------
N-axis Val= -0.67 Plg= 79.5 Azm = 328.8 ##########--------------------
P-axis Val= -3.77 Plg= 10.4 Azm = 154.9 ########---------- -----
Best Double Couple: Mo=4.10**26 Mw=7.0 ####----------- P --
nodal planes (strike/dip/slip): -----------
199.4/ 81.9/ -6.6 290.3/ 83.4/-171.8 Fit is GOOD (22% of 27 records)
----- End Included Message -----
Here is a typical mailing from NEIC--
From zirbes@gldfs.cr.usgs.gov Wed Nov 22 16:34:09 1995
Date: Wed, 22 Nov 95 16:05:45 MST
From: zirbes@gldfs.cr.usgs.gov (Madeleine Zirbes)
To: zirbes@gldfs.cr.usgs.gov
Subject: 22NOV95 EGYPT
Content-Length: 1392
95/11/22 04:15:11.54
EGYPT
Epicenter: 28.544 34.746
mb 6.2 MS 7.2
MOMENT TENSOR SOLUTION
Depth 20 No. of sta: 33
Moment Tensor; Scale 10**19 Nm
Mrr= 0.47 Mtt=-1.06
Mff= 0.58 Mrt= 1.38
Mrf=-0.59 Mtf=-2.53
Principal axes:
T Val= 3.08 Plg=27 Azm= 50
N 0.00 59 261
P -3.08 13 147
Best Double Couple:Mo=3.1*10**19
Mw=7.0
NP1:Strike=192 Dip=61 Slip= 10
NP2: 96 81 151
-------
----------#######
----------###########
-----------##############
------------########## ####
------------########### T #####
-----------############ #####
------------#####################
-----------######################
######-----######################
###########-------###############
###########----------------------
##########---------------------
##########---------------------
#########--------------------
#######------------ ---
######----------- P -
####-----------
-------
|