Brady 1D Seismic Velocity Model Ambient Noise Prelim
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.
Citation Formats
TY - DATA
AB - 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.
AU - J., Robert
DB - Geothermal Data Repository
DP - Open EI | National Renewable Energy Laboratory
DO - 10.15121/1148801
KW - seismic
KW - velocity model
KW - Bradys
KW - seismic velocity
KW - geothermal
KW - nevada
LA - English
DA - 2013/10/25
PY - 2013
PB - Lawrence Livermore National Laboratory
T1 - Brady 1D Seismic Velocity Model Ambient Noise Prelim
UR - https://doi.org/10.15121/1148801
ER -
J., Robert. Brady 1D Seismic Velocity Model Ambient Noise Prelim. Lawrence Livermore National Laboratory, 25 October, 2013, Geothermal Data Repository. https://doi.org/10.15121/1148801.
J., R. (2013). Brady 1D Seismic Velocity Model Ambient Noise Prelim. [Data set]. Geothermal Data Repository. Lawrence Livermore National Laboratory. https://doi.org/10.15121/1148801
J., Robert. Brady 1D Seismic Velocity Model Ambient Noise Prelim. Lawrence Livermore National Laboratory, October, 25, 2013. Distributed by Geothermal Data Repository. https://doi.org/10.15121/1148801
@misc{GDR_Dataset_262,
title = {Brady 1D Seismic Velocity Model Ambient Noise Prelim},
author = {J., Robert},
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.},
url = {https://gdr.openei.org/submissions/262},
year = {2013},
howpublished = {Geothermal Data Repository, Lawrence Livermore National Laboratory, https://doi.org/10.15121/1148801},
note = {Accessed: 2025-04-24},
doi = {10.15121/1148801}
}
https://dx.doi.org/10.15121/1148801
Details
Data from Oct 25, 2013
Last updated May 30, 2017
Submitted Oct 25, 2013
Organization
Lawrence Livermore National Laboratory
Contact
Robert J. Mellors
924.423.0578
Authors
Keywords
seismic, velocity model, Bradys, seismic velocity, geothermal, nevadaDOE Project Details
Project Name Monitoring EGS Stimulation and Reservoir Dynamics with InSAR and MEQ
Project Lead Lauren Boyd
Project Number EE0005510
