Computerized modeling of sedimentary systems [Libro electrónico] / editores: Jan Harff, Wolfram Lemke, Karl Stattegger
Harff, Jan [editor] | Lemke, Wolfram [editor/a] | Stattegger, Karl [editor/a].
Tipo de material: Libro en línea Editor: New York, New York, United States: Springer, c1999Descripción: xv, 452 páginas : ilustraciones mapas ; 24 centímetros.ISBN: 3540641092; 9783642083808 (Print); 9783662039021 (Online).Tema(s): Sedimentary basins -- Environmental aspects -- Computer simulation | Sedimentation and deposition -- Environmental aspects -- Computer simulationNota de acceso: Disponible para usuarios de ECOSUR con su clave de acceso Nota de bibliografía: Incluye bibliografía Número de sistema: 56454Contenidos:Mostrar Resumen:Tipo de ítem | Biblioteca actual | Colección | Signatura | Estado | Fecha de vencimiento | Código de barras |
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Libros | Biblioteca Electrónica Recursos en línea (RE) | Acervo General | Recurso digital | ECO400564549973 |
Incluye bibliografía
Chapter 1. Climatic, oceanographic and biological forcing of sedimentary systems.. Chapter 2. Trend and periodicity sedimentary record as a response to environmental changes.. Chapter 3. Space-time models of basin fill.. Bibliography
Disponible para usuarios de ECOSUR con su clave de acceso
Computerized modeling is a powerful tool to describe the complex interrelations between measured data and the dynamics of sedimentary systems. Complex interaction of environmental factors with natural variations and increasing anthropogenic intervention is reflected in the sedimentary record at varying scales. The understanding of these processes gives way to the reconstruction of the past and is a key to the prediction of future trends. Especially in cases where observations are limited and/or expensive, computer simulations may substitute for the lack of data. State-of-the-art research work requires a thorough knowledge of processes at the interfaces between atmosphere, hydrosphere, biosphere, and lithosphere, and is therefore an interdisciplinary approach. eng
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