1 We compute short-period, high-resolution surface wave slowness maps for central Asia using Bayesian tomography. We focus on the region between 69 degrees and 108 degrees E and 29 degrees and 54 degrees N and used seismograms from more than 1100 events. Using multiple-filter and phase-matched filter techniques, we measured the dispersion characteristics of the signals between 6 and 30 s period. These Rayleigh wave group velocity dispersion curves were used to compute high-resolution, half-degree cell size, slowness tomographic maps. Because short periods are primarily sensitive to upper crustal structures, the images display low velocities associated with the Tarim, Junggar, and Qaidam basins. Relatively high velocities are associated with mountainous tectonic features such as the Tian Shan. We validated our maps using dispersion curves from 640 events that were not used to construct the tomographic model. The model predictions show a significant variance reduction at short and intermediate periods ( 6 - 15 s) with respect to the prior model. Our model also shows 15% improvement in surface wave detection capability with respect to previous one-dimensional models. These high-resolution, short-period tomography maps can help improve regional magnitude estimations for construction of m(b): M-s discriminants. Moreover, the short-period surface wave tomographic results show unprecedented resolution that reveals greater geologic detail than has previously been achieved using surface waves and that give us insight into the shear velocity structure of the crust underlying this part of Asia.
Los Alamos Natl Lab, Los Alamos, NM 87545 USA. Penn State Univ, Dept Geosci, University Pk, PA 16802 USA. Univ Texas, Dept Geol Sci, El Paso, TX 79968 USA.
%0 Journal Article
%1 Maceira:2005
%A Maceira, M.
%A Taylor, S. R.
%A Ammon, C. J.
%A Yang, X. N.
%A Velasco, A. A.
%C WASHINGTON
%D 2005
%I AMER GEOPHYSICAL UNION
%J JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
%K BASIN; CENTRAL CHINA; DISPERSION EURASIA; MANTLE PHASE-VELOCITY; PLATEAU; SHEAR STRUCTURE; SURFACE-WAVES; TARIM TIAN-SHAN; TIBETAN UPPER VELOCITY WESTERN
%N B6
%P B06304
%R 10.1029/2004JB003429
%T High-resolution Rayleigh wave slowness tomography of central Asia
%V 110
%X 1 We compute short-period, high-resolution surface wave slowness maps for central Asia using Bayesian tomography. We focus on the region between 69 degrees and 108 degrees E and 29 degrees and 54 degrees N and used seismograms from more than 1100 events. Using multiple-filter and phase-matched filter techniques, we measured the dispersion characteristics of the signals between 6 and 30 s period. These Rayleigh wave group velocity dispersion curves were used to compute high-resolution, half-degree cell size, slowness tomographic maps. Because short periods are primarily sensitive to upper crustal structures, the images display low velocities associated with the Tarim, Junggar, and Qaidam basins. Relatively high velocities are associated with mountainous tectonic features such as the Tian Shan. We validated our maps using dispersion curves from 640 events that were not used to construct the tomographic model. The model predictions show a significant variance reduction at short and intermediate periods ( 6 - 15 s) with respect to the prior model. Our model also shows 15% improvement in surface wave detection capability with respect to previous one-dimensional models. These high-resolution, short-period tomography maps can help improve regional magnitude estimations for construction of m(b): M-s discriminants. Moreover, the short-period surface wave tomographic results show unprecedented resolution that reveals greater geologic detail than has previously been achieved using surface waves and that give us insight into the shear velocity structure of the crust underlying this part of Asia.
@article{Maceira:2005,
abstract = {[1] We compute short-period, high-resolution surface wave slowness maps for central Asia using Bayesian tomography. We focus on the region between 69 degrees and 108 degrees E and 29 degrees and 54 degrees N and used seismograms from more than 1100 events. Using multiple-filter and phase-matched filter techniques, we measured the dispersion characteristics of the signals between 6 and 30 s period. These Rayleigh wave group velocity dispersion curves were used to compute high-resolution, half-degree cell size, slowness tomographic maps. Because short periods are primarily sensitive to upper crustal structures, the images display low velocities associated with the Tarim, Junggar, and Qaidam basins. Relatively high velocities are associated with mountainous tectonic features such as the Tian Shan. We validated our maps using dispersion curves from 640 events that were not used to construct the tomographic model. The model predictions show a significant variance reduction at short and intermediate periods ( 6 - 15 s) with respect to the prior model. Our model also shows 15% improvement in surface wave detection capability with respect to previous one-dimensional models. These high-resolution, short-period tomography maps can help improve regional magnitude estimations for construction of m(b): M-s discriminants. Moreover, the short-period surface wave tomographic results show unprecedented resolution that reveals greater geologic detail than has previously been achieved using surface waves and that give us insight into the shear velocity structure of the crust underlying this part of Asia.},
added-at = {2010-08-12T23:06:12.000+0200},
address = {WASHINGTON},
author = {Maceira, M. and Taylor, S. R. and Ammon, C. J. and Yang, X. N. and Velasco, A. A.},
author-address = {Los Alamos Natl Lab, Los Alamos, NM 87545 USA. Penn State Univ, Dept Geosci, University Pk, PA 16802 USA. Univ Texas, Dept Geol Sci, El Paso, TX 79968 USA.},
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bdsk-url-1 = {http://dx.doi.org/10.1029/2004JB003429},
biburl = {https://www.bibsonomy.org/bibtex/2ee76ab6c08c8f1eb959bd4580f1ba8b5/jkmacc},
cited-reference-count = {60},
date-added = {2010-04-07 02:08:41 -0600},
date-modified = {2010-04-07 02:08:41 -0600},
document-type = {Article},
doi = {10.1029/2004JB003429},
e-mail-address = {mmaceira@lanl.gov taylor@lanl.gov cammon@geosc.psu.edu xyang@lanl.gov velasco@geo.utep.edu},
interhash = {272dd2e894259bc3ead3f792a93a0f66},
intrahash = {ee76ab6c08c8f1eb959bd4580f1ba8b5},
isi = {ISI:000229965900002},
isi-document-delivery-number = {937ZA},
iso-source-abbreviation = {J. Geophys. Res.-Solid Earth},
issn = {0148-0227},
journal = {JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH},
keywords = {BASIN; CENTRAL CHINA; DISPERSION EURASIA; MANTLE PHASE-VELOCITY; PLATEAU; SHEAR STRUCTURE; SURFACE-WAVES; TARIM TIAN-SHAN; TIBETAN UPPER VELOCITY WESTERN},
language = {English},
month = Jun,
number = {B6},
page-count = {21},
pages = {B06304},
publication-type = {J},
publisher = {AMER GEOPHYSICAL UNION},
publisher-address = {2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA},
reprint-address = {Maceira, M, Los Alamos Natl Lab, EES-11,MS D443, Los Alamos, NM 87545 USA.},
source = {J GEOPHYS RES-SOLID EARTH},
subject-category = {Geochemistry & Geophysics},
times-cited = {3},
timestamp = {2010-08-12T23:06:12.000+0200},
title = {High-resolution Rayleigh wave slowness tomography of central Asia},
volume = 110,
year = 2005
}