Modelling grain-size distributions. A comparison of two models and their numerical solution

Tectonophysics

Volumn 320, Issue 3-4, 2000, Pages 347-373

  Den Bezemer, Taco ^a   Kooi, Henk ^a   Kranenborg, Jurjen ^a   Cloetingh, Sierd ^a  

^a VU UNIVERSITY AMSTERDAM   (Netherlands)

Author keywords

[No Author keywords available]

Indexed keywords

COMPARATIVE STUDY; GRAIN SIZE; MODELING; SIZE DISTRIBUTION;

EID: 0033748045     PISSN: 00401951     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0040-1951(00)00041-X     Document Type: Article

References (24)

1. Quantitative sedimentary basin modelling
2. Application of a diffusion-erosion model to alluvial channels which degrade due to baselevel lowering
3. The downstream gradation of particle sizes in the Squamish River, British Columbia
4. Quantitative dynamic stratigraphy: A workshop a philosophy a methodology
5. Field evidence for rapid downstream fining of river gravels through selective transport
6. STRATA: Freeware for analyzing classic stratigraphic problems
7. Computer modeling of tectonics, enstacy, and sedimentation using the Macintosh
8. Quantitative geologic modeling of siliclastic rock sequences and their seismic expression
9. Morphology of a delta prograding by bulk sediment transport
10. Escarpment evolution on high-elevation rifted margins: Insights derived from surface processes model that combines diffusion, advection and reaction
11. The effects of abrasion on the size, shape and roundness of rock fragments
12. Stratigraphic simulation of sedimentary basins: Concepts and calibration
13. Subsidence and gravel transport in alluvial basins
14. Self-formed straight rivers with equilibrium banks and mobile bed, Part 2, the gravel river
15. Relationship between eustacy and stratigraphic sequences of passive margins
16. Application of a dual-lithology, depth-dependent diffusion equation in stratigraphic simulation
17. The composition of recent alluvial gravels in Alberta River beds: Alberta
18. Abrasion in place: A mechanism for rounding and size reduction of coarse sediments in rivers