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Titlebook: Dating Torrential Processes on Fans and Cones; Methods and Their Ap Michelle Schneuwly-Bollschweiler,Markus Stoffel,Fl Book 2013 Springer S

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發(fā)表于 2025-3-26 23:09:35 | 只看該作者
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發(fā)表于 2025-3-27 03:16:30 | 只看該作者
P. Lebrun,L. Grivet,L. Baudouinlains, etc.) for purposes of hazard assessment and mitigation commonly requires greater dating precision than is available through radiocarbon dating or other methods. Ages of trees growing on landform surfaces have been used in a number of studies to estimate the time of landform creation or surfac
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發(fā)表于 2025-3-27 16:40:52 | 只看該作者
Ajit Pratap Singh,Deepali Joharitial. This development mirrors the contributions made in investigations of other depositional environments since invention of the technique in the 1950s (Cook and van der Plicht 2007; Jull 2007). Radiocarbon dating involves measuring the amount of the radioisotope .C preserved in fossil organic mate
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發(fā)表于 2025-3-27 22:15:49 | 只看該作者
978-94-007-9986-8Springer Science+Business Media Dordrecht 2013
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發(fā)表于 2025-3-28 05:57:40 | 只看該作者
Book 2013impact of past and potential future climate change on torrential processes. The book has a clear focus on the practical applications of these methods, complemented by case studies. The limits of each dating method in case of excessive natural and human interventions on fans and cones are shown.
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發(fā)表于 2025-3-28 08:15:16 | 只看該作者
,Dating Past Events on Fans and Cones – An Introduction,Moreover cones are also formed by scree deposits, rock avalanches, slope-type debris flows, mudflows, lahars, landslides, sheet floods and other forms of rapid mass movements. Alluvial fans and debris cones are typically located in mountain fronts and develop at the base of headwater basins. The ape
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發(fā)表于 2025-3-28 12:26:56 | 只看該作者
Processes of Sediment Supply to Alluvial Fans and Debris Conesto enormous fluvial “megafans” (Harvey 2011). Within the context of this book the focus is on the intermediate scale, debris cones to “classic alluvial fans”. Such landforms are found in three main settings (Harvey 2010): mountain-front, intra-montane, and tributary-junction settings. They occur in
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