Hi Asthon,
So far, I think we can compute the CC with a minimum of 3 stations (Am I right Thomas?).
What I did for Costa Rica was computing seismic velocity variations for selected station
pairs instead of the average seismic velocity change for the whole N array. You can adapt
the scripts for this...
It would be really cool if we can implement sub-arrays from the N stations and monitoring
these sub-arrays and compare results.
Changing gears a bit:
** Another cool idea that I am throwing here is to implement a tool/ function that allow
us to use the final Green’s functions as virtual earthquakes!! So we can perform moment
tensor inversions (for instance) and make some seismic hazard analysis.
Cheers;
-Esteban
On Oct 21, 2016, at 5:00 AM,
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Today's Topics:
1. selective pairs (Flinders, Ashton)
----------------------------------------------------------------------
Message: 1
Date: Thu, 20 Oct 2016 08:47:50 -0700
From: "Flinders, Ashton" <aflinders(a)usgs.gov>
To: "Python Package for Monitoring Seismic Velocity Changes using
Ambient Seismic Noise" <msnoise(a)mailman-as.oma.be>
Subject: [MSNoise] selective pairs
Message-ID:
<CAPbWHEMzu7y40649A5TesRz9i80yjn9t6KRwnAzRhUzAAP04JA(a)mail.gmail.com>
Content-Type: text/plain; charset="UTF-8"
Hi all,
I was wondering if anyone had already implemented something like this. I'd
like to be able to select which CC pairs I calculated, instead of all
combinations. My reasoning is, I want to use this for monitoring changes
associated with a potential magma reservoir, and only want to look at ray
paths that cross the caldera.
Thanks!
-ashton
--
Ashton F. Flinders, Ph.D
U.S. Geological Survey
345 Middlefield Road
Menlo Park, CA 94025
(650) 329-5050
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