Abstract
Alluvial fans and debris cones are important buffers in the sediment cascade from mountains to the sea. Interactions between tectonic, climate, and base-level controls often render fans and cones dynamic geomorphic features – even on timescales of millennia and beyond (Harvey 2010). Unraveling such dynamics has proven difficult mainly because establishing chronologies for fans and cones is challenging: Buried organic remains are usually scare (Chiverrell and Jakob 2012, this volume), dendrochronology and lichenometry (Schneuwly-Bollschweiler and Stoffel 2012, this volume; Jomelli 2012, this volume) will often be limited to cone and fan surfaces and help accessing the recent past only (Lang et al. 1999), and rarely are tephra layers preserved or synsedimentary carbonates developed that would permit radiometric dating. Luminescence dating can offer an alternative as it allows determining the time when sediments were laid down. But limitations exist that are related to (i) limited exposure of sediment grains to daylight during the short and rapid transport of many fan deposits and (ii) low luminescence sensitivity of quartz from many high mountain environments. After a brief introduction on luminescence dating techniques, an overview of relevant dating applications is given and the possibilities and limitations of applying luminescence dating to alluvial fan and debris cones are discussed.
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Lang, A. (2013). Luminescence Dating of Alluvial Fans and Cones. In: Schneuwly-Bollschweiler, M., Stoffel, M., Rudolf-Miklau, F. (eds) Dating Torrential Processes on Fans and Cones. Advances in Global Change Research, vol 47. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-4336-6_18
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