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Geodynamic evolution of sedimentary basins proceedings of the international symposium held in Moscow, May 18-23, 1992 by

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Published by Editions Technip in Paris .
Written in English


  • Sedimentary basins -- Congresses.,
  • Petroleum -- Geology -- Congresses.,
  • Natural gas -- Geology -- Congresses.,
  • Geodynamics -- Congresses.

Book details:

Edition Notes

Statementedited by F. Roure ... [et al.] ; sponsoring, Committee on Fossil Fuels of the International Union of Geological Sciences (IUGS) ... [et al.].
ContributionsRoure, François., International Union of Geological Sciences. Committee on Fossil Fuels., Institut français du pétrole., Institut geologii i razrabotki gori͡u︡chikh iskopaemykh (Russia), Vsesoi͡u︡znyĭ nauchno-issledovatelʹskiĭ geologorazvedochnyĭ nefti͡a︡noĭ institut (Soviet Union)
LC ClassificationsQE615 .G46 1996
The Physical Object
Paginationxi, 453 p. :
Number of Pages453
ID Numbers
Open LibraryOL728055M
ISBN 102710806924
LC Control Number97116842

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Geodynamics is a subfield of geophysics dealing with dynamics of the applies physics, chemistry and mathematics to the understanding of how mantle convection leads to plate tectonics and geologic phenomena such as seafloor spreading, mountain building, volcanoes, earthquakes, faulting and so on. It also attempts to probe the internal activity by measuring magnetic fields, gravity, and. Study of sedimentary basins. The study of sedimentary basins as a specific entity in themselves is often referred to as basin modelling or sedimentary basin analysis. The need to understand the processes of basin formation and evolution are not restricted to the purely academic. This book focuses on the strong relation between the tectonic evolution of the Southernmost Andes and their closest southern neighbors, the Scotia Sea and Antarctica. Some episodes are related to processes of global significance such as the opening of the Drake Passage, which is somehow linked to Late Cenozoic cooling. Regional seismic surveys and drilling data from the eastern part of the West Siberian plate west of the Yenisei River reveal thick moderately deformed Neoproterozoic and Early Paleozoic sediments that belong to an ancient basin of Fore-Yenisei under the Mesozoic-Cenozoic by: 1.