Sedimentology And Sedimentary Basins. From Turbulence To Tectonics

Mike Leeder

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Mike Leeder - Sedimentology And Sedimentary Basins. From Turbulence To Tectonics.
Sedimentology is a core discipline of earth and environmental sciences. It enquires the origins, transport and deposition of mineral sediment on the Earth's... Lire la suite
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Résumé

Sedimentology is a core discipline of earth and environmental sciences. It enquires the origins, transport and deposition of mineral sediment on the Earth's surface. The subject is a link between positive effects arising from the building of relief by tectonics and the negative action of denudation in drainage catchments and tectonic subsidence in sedimentary basins. The author addresses the principles of the subject, emphasising the advantages of a general science approach and the importance of understanding modern processes. Sedimentology and Sedimentary Basins is not an encyclopaedia, but attempts to stimulate interdisciplinary thought across the whole subject area and related disciplines. The book has been designed to meet the needs of earth and environmental science undergraduates.

Sommaire

    • Origin and Types of Sediment Grains
    • User's Guide to Sedimentological Fluid Dynamics
    • Sediment Transport and Sedimentary Structures
    • External Controls on Sediment Derivation, Transport and Deposition
    • Sediment Deposition, Environments and Facies in Continental Environments
    • Sediment Deposition, Environments and Facies in Marine Environments
    • Sedimentology in Sedimentary Basins.

Caractéristiques

  • Date de parution
    01/10/1999
  • Editeur
  • ISBN
    0-632-04976-6
  • EAN
    9780632049769
  • Présentation
    Broché
  • Nb. de pages
    592 pages
  • Poids
    1.695 Kg
  • Dimensions
    19,0 cm × 24,7 cm × 3,5 cm

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À propos de l'auteur

Biographie de Mike Leeder

Mike Leeder is currently at the School of Environmental Sciences, University of East Anglia, Norwich. Previously he was at the School of Earth Sciences, University of Leeds. Mike believes that the first step in sedimentological problem-solving comes from field observations, a grasp of basic physics or chemistry comes second, and the application of simple mathematics third.

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