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Title: Brady 1D seismic velocity model ambient noise prelim

Abstract

Preliminary 1D seismic velocity model derived from ambient noise correlation. 28 Green's functions filtered between 4-10 Hz for Vp, Vs, and Qs were calculated. 1D model estimated for each path. The final model is a median of the individual models. Resolution is best for the top 1 km. Poorly constrained with increasing depth.

Authors:
Publication Date:
Other Number(s):
262
DOE Contract Number:  
EE0005510
Product Type:
Dataset
Research Org.:
USDOE Geothermal Data Repository (United States); Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
Sponsoring Org.:
USDOE Office of Energy Efficiency and Renewable Energy (EERE), Renewable Power Office. Geothermal Technologies Office
Subject:
15 Geothermal Energy
Keywords:
seismic; velocity model; Bradys
OSTI Identifier:
1148801
DOI:
https://doi.org/10.15121/1148801

Citation Formats

Mellors, Robert J. Brady 1D seismic velocity model ambient noise prelim. United States: N. p., 2013. Web. doi:10.15121/1148801.
Mellors, Robert J. Brady 1D seismic velocity model ambient noise prelim. United States. doi:https://doi.org/10.15121/1148801
Mellors, Robert J. 2013. "Brady 1D seismic velocity model ambient noise prelim". United States. doi:https://doi.org/10.15121/1148801. https://www.osti.gov/servlets/purl/1148801. Pub date:Fri Oct 25 00:00:00 EDT 2013
@article{osti_1148801,
title = {Brady 1D seismic velocity model ambient noise prelim},
author = {Mellors, Robert J.},
abstractNote = {Preliminary 1D seismic velocity model derived from ambient noise correlation. 28 Green's functions filtered between 4-10 Hz for Vp, Vs, and Qs were calculated. 1D model estimated for each path. The final model is a median of the individual models. Resolution is best for the top 1 km. Poorly constrained with increasing depth.},
doi = {10.15121/1148801},
journal = {},
number = ,
volume = ,
place = {United States},
year = {2013},
month = {10}
}