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Application of second arrivals in seismic tomography inversion for the crustal structure study

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Standard seismic tomography is based on the first arrival refracted Pg- and Pn-waves travel times and as a result gives a smooth model of the structure. Sharp discontinuities, particularly the Moho, as well as lower crust, are poorly constraint. The paper presents a modification of the standard method which allows to use later arrivals of crustal Pcr waves together with the first arrival travel times. They give better coverage by rays and better model for the whole crust. Results are illustrated by synthetic models and interpretation of experimental data from POLONAISE'97 profile P4.
Rocznik
Strony
13--26
Opis fizyczny
Bibliogr. 12 poz.
Twórcy
  • Institute of Geophysics, Warsaw University, Pasteura 7, 02-093 Warszawa, Poland
autor
  • Institute of Geophysics, Warsaw University, Pasteura 7, 02-093 Warszawa, Poland
Bibliografia
  • Červený, v., and I. Pšenčik, 1983, 2-D seismic ray tracing package SEIS83 (software pack¬age), Charles University, Prague.
  • Grad, M., et al., 2003, Crustal structure of the Trans-European suture zone region along POLONAISE'97 seismic profile P4, J. Geophys. Res. 108 (Bll), 2541, doi: 10.1029/ 2003JB002426.
  • Guterch, A., M. Grad, H. Thybo, G.R. Keller and POLONAISE Working Group, 1999, POLONAISE'97 - International seismic experiment between Precambrian and Varis-can Europe in Poland, Tectonophysics 314, 101-121.
  • Hobro, J.W.D., 1999, Joint interface and velocity estimation in three dimensions (JIVE3D), University of Cambridge Press, Cambridge UK.
  • Hole, J.R., 1992, Non-linear high resolution three-dimensional seismic travel time tomogra¬phy, J. Geophys. Res. 97, 6553-6562.
  • Komminaho, K., 1993, Software manual for programs MODEL and XRAYS-a graphical inter¬face for SEIS83 program package, Department of Geophysics, University of Oulu, Finland, Report 20,31 pp.
  • Środa, P., 2000, 3-D modelling of the crustal structure in the contact zone between Antarctic Peninsula and South Pacific from seismic data, Ph.D. Thesis, Institute of Geophysics, Polish Academy of Science, 112 pp. (unpublished).
  • Środa, P., W. Czuba, M. Grad, A. Guterch, E. Gaczyński and POLONAISE Working Group, 2002, Three-dimensional seismic modelling of crustal structure in the TESZ region based on POLONAISE'97 data, Tectonophysics 360, 169-185
  • Vidale, I.E., 1990, Finite-difference calculation of travel times in three dimensions, Geophys¬ics 55, 521-526.
  • Zelt, C.A., 1994, ZPLOT - An interactive plotting and picking program for seismic data, Bul-lard Lab., University of Cambridge Press, Cambridge UK.
  • Zelt, C.A., 1998, Lateral velocity resolution from 3-D seismic refraction data, Geophys. J. Intern. 135, 1101-1112.
  • Zelt, C.A., and D.A. Forsyth, 1994, Modelling wide-angle seismic data for crustal structure: southeastern Grenville province, J. Geophys. Res. 99, 11687-11704
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL7-0009-0004
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