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• W2324253764 abstract "Other| September 01, 1998 ET1D: New One Dimensional P- and S-Wave Velocity Models for the Eastern Tennessee Seismic Zone Gordana Vlahovic; Gordana Vlahovic Department of Geology UNC Chapel Hill Chapel Hill, North Carolina 27599-3315 (G. V., C.A.P.) Search for other works by this author on: GSW Google Scholar Christine A. Powell; Christine A. Powell Department of Geology UNC Chapel Hill Chapel Hill, North Carolina 27599-3315 (G. V., C.A.P.) Search for other works by this author on: GSW Google Scholar Martin C. Chapman; Martin C. Chapman Department of Geological Sciences Virginia Polytechnic Institute and State University Blacksburg, Virginia 24061 (M.C.C.) Search for other works by this author on: GSW Google Scholar Matthew Sibol Matthew Sibol ENSCO, Inc. 445 Pineda Court Melbourne, Florida 32940 (M.S.) Search for other works by this author on: GSW Google Scholar Seismological Research Letters (1998) 69 (5): 441–449. https://doi.org/10.1785/gssrl.69.5.441 Article history first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Gordana Vlahovic, Christine A. Powell, Martin C. Chapman, Matthew Sibol; ET1D: New One Dimensional P- and S-Wave Velocity Models for the Eastern Tennessee Seismic Zone. Seismological Research Letters 1998;; 69 (5): 441–449. doi: https://doi.org/10.1785/gssrl.69.5.441 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search nav search search input Search input auto suggest search filter All ContentBy SocietySeismological Research Letters Search Advanced Search Abstract A joint hypocenter-velocity inversion for the eastern Tennessee seismic zone (ETSZ) has produced one-dimensional P- and S-wave velocity models for the upper crust. The models, called ET1D, are based upon P- and S-wave arrival times from 492 earthquakes recorded by regional seismic networks. P- and S-wave velocity models were computed independently. The final 1D velocity models display a systematic increase of velocity with depth and a stable Vp/Vs ratio between 1.72 and 1.74. Relocation using ET1D reduced scatter in hypocenter locations, primarily through changes in focal depth. Relocated hypocenters also had reduced RMS residuals, horizontal errors, and vertical errors relative to values obtained with the velocity model presently used for hypocenter determinations in the ETSZ. ET1D was extended to include the entire crust to allow this model to be used for routine hypocenter determinations in the ETSZ. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not currently have access to this article." @default.
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• W2324253764 title "ET1D: New One Dimensional P- and S-Wave Velocity Models for the Eastern Tennessee Seismic Zone" @default.
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