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dc.contributor.author Lienert, Barry R.
dc.contributor.author Frazer, L. Neil
dc.contributor.author Rudman, Albert J.
dc.date.accessioned 2013-03-06T18:24:51Z
dc.date.available 2013-03-06T18:24:51Z
dc.date.issued 1986
dc.identifier.citation Lienert, Barry R., Frazer, L. Neil and Rudman, Albert J., 1986, Evaluation of Seismometer Arrays for Earthquake Location.Indiana Geological Survey 11, 53 p., 9 fig. en
dc.identifier.uri http://hdl.handle.net/2022/15326
dc.description.abstract Program HYPOERR evaluates the performance of a small network of arbitrary seismic arrays in determining coordinates and times of seismic events. A linearized inversion following the method of Uhrhammer (1980)is performed for a layered velocity structure by determining the eigenvalues and eigenvectors of the partial derivatives of travel time for P and/or S phases with respect to hypocenter position and origin time for each station in the array. A series of covariance matrices is then obtained to evaluate statistical errors for a specified grid of hypocenter locations at any given depth. Contour plots can then be made of the matrix elements by using standard contouring software. Examples are given for ( 1) the case of a hypothetical quadrapartite array and (2) an actual eight-station ocean-bottom seismometer array deployed around the 95.5° W. Galapagos propagating-rift zone. en
dc.language.iso en_US en
dc.publisher Indiana Geological Survey en
dc.relation.ispartofseries Occasional Paper;11
dc.rights This work is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-sa/2.5/ or send a letter to Creative Commons, 543 Howard Street, 5th Floor, San Francisco, California, 94105, USA. en
dc.subject Seismic Array, Earthquake Location, Galapagos Location,Geophysical Computer Programs en
dc.title Evaluation of Seismometer Arrays for Earthquake Location en
dc.title.alternative Geophysical Computer Program 11 en
dc.type Technical Report en


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