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NEIC U.S. Geological Survey, Box 25046, Mail Stop 966Denver Federal Center, Denver, Colorado 80225engdahl{at}gldfs.cr.usgs.gov
Department of Earth, Atmospheric and Planetary Sciences Massachusetts Institute of Technology, Rm 54-514, Cambridge, Massachusetts 02139
Abstract
We relocate nearly 100,000 events that occurred during the period 1964 to 1995 and are well-constrained teleseismically by arrival-time data reported to the International Seismological Centre (ISC) and to the U.S. Geological Survey's National Earthquake Information Center (NEIC). Hypocenter determination is significantly improved by using, in addition to regional and teleseismic P and S phases, the arrival times of PKiKP, PKPdf, and the teleseismic depth phases pP, pwP, and sP in the relocation procedure. A global probability model developed for later-arriving phases is used to independently identify the depth phases. The relocations are compared to hypocenters reported in the ISC and NEIC catalogs and by other sources. Differences in our epicenters with respect to ISC and NEIC estimates are generally small and regionally systematic due to the combined effects of the observing station network and plate geometry regionally, differences in upper mantle travel times between the reference earth models used, and the use of later-arriving phases. Focal depths are improved substantially over most other independent estimates, demonstrating (for example) how regional structures such as downgoing slabs can severely bias depth estimation when only regional and teleseismic P arrivals are used to determine the hypocenter. The new data base, which is complete to about Mw 5.2 and includes all events for which moment-tensor solutions are available, has immediate application to high-resolution definition of Wadati-Benioff Zones (WBZs) worldwide, regional and global tomographic imaging, and other studies of earth structure.
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R. L. Hermanns, S. Niedermann, A. V. Garcia, J. S. Gomez, and M. R. Strecker Neotectonics and catastrophic failure of mountain fronts in the southern intra-Andean Puna Plateau, Argentina Geology, July 1, 2001; 29(7): 619 - 622. [Abstract] [Full Text] [PDF]
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W.-P. Chen and M. R. Brudzinski Evidence for a Large-Scale Remnant of Subducted Lithosphere Beneath Fiji Science, June 29, 2001; 292(5526): 2475 - 2479. [Abstract] [Full Text] [PDF]
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Improving Global Seismic Event Locations Using Source-Receiver Reciprocity Bulletin of the Seismological Society of America, June 1, 2001; 91(3): 594 - 603.
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S. M. Peacock Are the lower planes of double seismic zones caused by serpentine dehydration in subducting oceanic mantle? Geology, April 1, 2001; 29(4): 299 - 302. [Abstract] [Full Text] [PDF]
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Position of the Disastrous 1999 Puebla Earthquake in the Seismotectonic Pattern of Mexico Bulletin of the Seismological Society of America, June 1, 2000; 90(3): 786 - 789.
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Improving Sparse Network Seismic Location with Bayesian Kriging and Teleseismically Constrained Calibration Events Bulletin of the Seismological Society of America, February 1, 2000; 90(1): 199 - 211.
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The Use of Waveform Shapes to Automatically Determine Earthquake Focal Depth Bulletin of the Seismological Society of America, February 1, 2000; 90(1): 248 - 254.
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P. G. Richards, X. Song, A. Li;, and A. Souriau; Detecting Possible Rotation of Earth's Inner Core Science, November 13, 1998; 282(5392): 1227a - 1227. [Full Text]
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