HVTFA - ellipticity inversions
Posted: Tue Jul 02, 2024 7:10 am
Hi Marc,
Posting here as per your advice.
I hope this email finds you well. I have been a Geopsy user for quite some time now but only restricted to HVSR processing. I am now exploring how to invert fundamental mode rayleigh wave ellipticity since I am soon to work on glacial ice thickness estimates and would like to have a go at HVTFA. With this, I just want to ask a couple of questions or clarifications rather regarding the entire process to produce a 1D shear velocity profile, particularly in max2curve and some of the script. Figures here will probably be incorrect (test data) but for the sake of visualization, I have included them here.
1. After loading the .max file into max2curve, the curve at the right window is essentially the fundamental mode Rayleigh wave ellipticity forward model I believe?
2. From here, we pick either left flank, right flank (or a combination), or the entire curve itself and save it as a multi-column file. Or do we just resample the existing curve into the left or right flanks such that the standard deviations are not lost? Here is the right flank as an example:
3. Say we proceeded with the picked right flank, load the curve into Dinver.
4. The resulting output of ellipticity (colored lines) are the numerical forward models fitting the experimental forward model?
5. And to extract the best fitting forward model after saving the report file, the script to use is:
gpdcreport name.report -best 1 | gpell -abs
I guess ultimately, I would like to produce something similar to the output of Knapmeyer-Endrun et al. (2017) https://link.springer.com/article/10.10 ... 016-0300-1:
I feel like I have been stuck in this process and would be really thankful for your inputs and comments regarding HVTFA.
Thank you so much for your time!
Best regards,
Leandro Aque
Posting here as per your advice.
I hope this email finds you well. I have been a Geopsy user for quite some time now but only restricted to HVSR processing. I am now exploring how to invert fundamental mode rayleigh wave ellipticity since I am soon to work on glacial ice thickness estimates and would like to have a go at HVTFA. With this, I just want to ask a couple of questions or clarifications rather regarding the entire process to produce a 1D shear velocity profile, particularly in max2curve and some of the script. Figures here will probably be incorrect (test data) but for the sake of visualization, I have included them here.
1. After loading the .max file into max2curve, the curve at the right window is essentially the fundamental mode Rayleigh wave ellipticity forward model I believe?
2. From here, we pick either left flank, right flank (or a combination), or the entire curve itself and save it as a multi-column file. Or do we just resample the existing curve into the left or right flanks such that the standard deviations are not lost? Here is the right flank as an example:
3. Say we proceeded with the picked right flank, load the curve into Dinver.
4. The resulting output of ellipticity (colored lines) are the numerical forward models fitting the experimental forward model?
5. And to extract the best fitting forward model after saving the report file, the script to use is:
gpdcreport name.report -best 1 | gpell -abs
I guess ultimately, I would like to produce something similar to the output of Knapmeyer-Endrun et al. (2017) https://link.springer.com/article/10.10 ... 016-0300-1:
I feel like I have been stuck in this process and would be really thankful for your inputs and comments regarding HVTFA.
Thank you so much for your time!
Best regards,
Leandro Aque