<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>J. Xia</dc:contributor>
  <dc:contributor>J. Liu</dc:contributor>
  <dc:contributor>Q. Liu</dc:contributor>
  <dc:contributor>S. Xu</dc:contributor>
  <dc:creator>Y. Luo</dc:creator>
  <dc:date>2007</dc:date>
  <dc:description>Joint inversion of multimode surface waves for estimating the shear (S)-wave velocity has received much attention in recent years. In this paper, we first analyze sensitivity of phase velocities of multimodes of surface waves for a six-layer earth model, and then we invert surface-wave dispersion curves of the theoretical model and a real-world example. Sensitivity analysis shows that fundamental mode data are more sensitive to the S-wave velocities of shallow layers and are concentrated on a very narrow frequency band, while higher mode data are more sensitive to the parameters of relatively deeper layers and are distributed over a wider frequency band. These properties provide a foundation of using a multimode joint inversion to define S-wave velocities. Inversion results of both synthetic data and a real-world example demonstrate that joint inversion with the damped least-square method and the singular-value decomposition technique to invert high-frequency surface waves with fundamental and higher mode data simultaneously can effectively reduce the ambiguity and improve the accuracy of S-wave velocities. ?? 2007.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/j.jappgeo.2007.02.004</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Joint inversion of high-frequency surface waves with fundamental and higher modes</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>