Modelling converted seismic waveforms in isotropic and anisotropic 1-D gradients: discontinuous versus continuous gradient representations

This is the latest version of this eprint.

Angus, DA and Thomson, CJ (2012) Modelling converted seismic waveforms in isotropic and anisotropic 1-D gradients: discontinuous versus continuous gradient representations. Studia Geophysica et Geodaetica, 56 (2). 383 - 409. ISSN 0039-3169

Abstract

Metadata

Authors/Creators:
  • Angus, DA
  • Thomson, CJ
Copyright, Publisher and Additional Information: (c) 2012, Springer. This is an author produced version of a paper published in Studia Geophysica et Geodaetica. Uploaded in accordance with the publisher's self-archiving policy. The final publication is available at Springer via http://dx.doi.org/10.1007/s11200-011-1350-1
Dates:
  • Published: 2012
Institution: The University of Leeds
Academic Units: The University of Leeds > Faculty of Environment (Leeds) > School of Earth and Environment (Leeds)
Depositing User: Symplectic Publications
Date Deposited: 27 Mar 2014 14:37
Last Modified: 29 Mar 2018 04:34
Published Version: http://dx.doi.org/10.1007/s11200-011-1350-1
Status: Published
Publisher: Springer Verlag
Identification Number: https://doi.org/10.1007/s11200-011-1350-1

Available Versions of this Item

Share / Export

Statistics