By Adrian M. Harvey, Anne E. Mather, Martin R. Stokes
Alluvial fanatics are vital sedimentary environments. They capture sediment brought from mountain resource components, and exert a big keep watch over at the supply of sediment to downstream environments, to axial drainages and to sedimentary basins. they keep a delicate list of environmental swap in the mountain resource parts. Alluvial fan geomorphology and sedimentology replicate not just drainage basin measurement and geology, yet switch in line with tectonic, climatic and base-level controls. one of many demanding situations dealing with alluvial fan study is to unravel how those gross controls are mirrored in alluvial fan dynamics and to use the result of reviews of contemporary fan approaches and Quaternary lovers to the knowledge of sedimentary sequences within the rock list. This quantity contains papers according to up to date examine, and specializes in 3 topics: alluvial fan strategies, dynamics of Quaternary alluvial fanatics and fan sedimentary sequences. Linking the papers is an emphasis at the controls of fan geomorphology, sedimentology and dynamics. this offers a foundation for integration among geomorphological and sedimentological techniques, and an knowing how fluvial platforms reply to tectonic, climatic and base-level changes.Also to be had: Submarine Slope structures - ISBN 1862391777 restrained Turbidite structures - ISBN 1862391491 Deep-water Sedimentation within the Alpine Basie of SE France - ISBN 1862391483
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Extra resources for Alluvial fans: geomorphology, sedimentology, dynamics
Bulletin of the Geological Society of America, 83, 2073-2098. IGME. 1977. Geological Map of Gythion 1:50 000 Scale. Institute of Geological and Mineral Exploration, Athens. IGME. 1983. Geological Map of Xilocambion, 1:50000 Scale. Institute of Geological and Mineral Exploration, Athens. , BERKHEMER, H. & BUTTNER, D. 1978. Structure and geodynamic evolution of the Aegean region. , ROEDER, D. & SCHMIDT, K. (eds) Alps, Alpennines and Hellenides. Schweizerbart'sche Verlagsbuchhandlung, Stuttgart, 536-564.
Pportedg ...... and cobbles Matrix-supportedsands (withcobbles) Finesand ~ Coarsesilt andfinesand Mediumto coarsesilt Medium - coarse sands with rare gravelstringers ~ Coarseningupwards Sedimentary ~ [~C ~ structures Pedogenic structures Horizontalbedding ~ TruncatedB-horizon ....... fabrics I~ . . . ed soil(clay. . . . ) Bloturbation Fig. 4b. Detailed lithostratigraphies associated with Qfl, Qf2, Qf3 and Qf4 segments of the study fans. and South Parorion fans), which was deposited by downwards percolating sediment-rich water (Pope 1995).
Yield of sediment in relation to mean annual precipitation. American Geophysical Union Transactions, 39, 1076-1084. M. COLLIER,R. 1988. Development of alluvial fans and fan deltas in neotectonic extensional settings: implications for the interpretation of basin-fills. In: NEMEC, W. J. (eds) Fan Deltas: Sedimentology and TectonicSettings. Blackie, London, 173-185. K. 1965. Clastic Sedimentation in Deep Springs Valley, California. US Geological Survey, Professional Paper, 352-F, 131-192. , ARMIJO, R.
Alluvial fans: geomorphology, sedimentology, dynamics by Adrian M. Harvey, Anne E. Mather, Martin R. Stokes