Lithosphere
Last modified December, 2013; irina@ign.ku.dk
Lithosphere
THE CONTINENTAL LITHOSPHERE
The site is being
updated,
12/2013
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Artemieva I.M., 2011.
The lithosphere:
An interdisciplinary
approach
.

Cambridge University Press,
Monograph,
794 pp., ISBN 9780521843966.

Download Contents and Preface
Download CV
Download papers
Download databases
Downloads of databases
SibCrust: CRUSTAL STRUCTURE OF SIBERIA
            (West Siberian Basin and Siberian Craton)
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University of Copenhagen
Øster Voldgade 10
Copenhagen DK-1350
Denmark
Email:
irina@ign.ku.dk
www.ign.ku.dk
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By downloading this database, you agree:
  1. to acknowledge the authorship by providing references to the original publications;
  2. do not use the databases for commercial purposes;
without a written permission from the author(s).
International Lithosphere
Programme ILP

  • SibCrust is a new digital crustal model for Moho depth and crustal structure in the West Siberian Basin
    and the Siberian Craton (60-140E, 50N–74N).

  • SibCrust model includes both Vp velocity and thickness of five crustal layers, including:
  • the sedimentary cover,
  • the upper crust,
  • the middle crust,
  • the lower crust,
  • the high-Vp lowermost crust,
  •    and the upper mantle Pn velocity.

  • Our compilation is based on digitization of all seismic profiles published since 1960 and sampled with a
    nominal interval of 50 km, which provides a dense regional data coverage.
  • Data quality has been assessed and quantitatively assigned to each profile based on acquisition and
    interpretation method and completeness of crustal model.
  • The database represents major improvement in coverage and resolution and includes depth to Moho,
    thickness and average P-wave velocity of five crustal layers and Pn velocity.
  • Exclusion of non-seismic data allows application of the database to potential field modeling.
Reference:
Cherepanova Yu., Artemieva I.M., Thybo H., Chemia Z., 2013.
Crustal structure of the Siberian Craton and the West Siberian Basin: An appraisal of existing seismic data.
Tectonophysics, 609, 154-183