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首页> 外文期刊>Quaternary Science Reviews: The International Multidisciplinary Review Journal >Extreme events in the sedimentary record of maar Lake Pavin: Implications for natural hazards assessment in the French Massif Central
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Extreme events in the sedimentary record of maar Lake Pavin: Implications for natural hazards assessment in the French Massif Central

机译:玛尔帕文湖沉积记录中的极端事件:对法国地块中部自然灾害评估的意义

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A set of sedimentary cores, high resolution swath bathymetry and subbottom profiler data provides new insights on sedimentary processes in meromictic maar Lake Pavin, France. Three sedimentary environments (i.e., littoral, plateau and basin) have been identified in the lake from sediment composition using bulk organic geochemistry and the analysis of hydroacoustic images. Various forms of rapidly deposited layers (RDLs) have been identified and radiocarbon dated. An up to date stratigraphy of sedimentary events matching coeval RDLs across the lake is presented and illustrates a wide range of natural hazards linked to Lake Pavin during the last 2000 years. In AD 600, a sudden lake outburst triggered a slump deposit along with a 9 m lake-level drop that drove shifts in sedimentary organic matter composition. Outside the lake, outburst flood deposits have been described downstream and provide sedimentary evidence for this event. The lake-level drop also favored the generation of gravity reworking processes, as shown by (1) a regional earthquake-triggered large slope failure on the plateau connected to a mass wasting deposit in the basin dated to AD 1300, and (2) a succession of turbidites in AD 1825 and AD 1860 contemporaneous to two historic earthquakes, suggesting that this lake is sensitive to earthquakes with a minimum epicentral intensity of V. Finally, past observations of lake water color changes in AD 1783 and AD 1936, similar to reports in other meromictic lakes, match iron-rich deposits identified in maar lake sediments and suggest that Lake Pavin could have undergone limnic eruptions. (C) 2016 Elsevier Ltd. All rights reserved.
机译:一组沉积岩心,高分辨率测深测深法和地下测井资料为法国淡马累帕尔湖的沉积过程提供了新见解。利用整体有机地球化学和水声图像分析,通过沉积物成分在湖中确定了三种沉积环境(即沿海,高原和盆地)。各种形式的快速沉积层(RDL)已被确定并标出了放射性碳。提出了与整个湖泊的RDL相匹配的沉积事件的最新地层学,说明了过去2000年与Pavin湖有关的各种自然灾害。公元600年,突然的湖水爆发触发了坍落沉积,湖水位下降了9 m,促使沉积有机物组成发生变化。在湖外,下游已描述了暴发性洪水沉积,并为该事件提供了沉积证据。湖泊水位下降也有利于重力重做过程的产生,如(1)所示,高原地区的一次地震引发的大边坡破坏与盆地中的大规模浪费沉积物有关,该沉积可追溯到公元1300年,(2)与两次历史性地震同时发生的公元1825和公元1860年的浊积岩相继表明,该湖对地震的敏感度最低,震中强度为V。在其他淡水湖泊中,匹配在玛尔湖沉积物中发现的富含铁的沉积物,这表明帕文湖可能已经发生了褐铁喷发。 (C)2016 Elsevier Ltd.保留所有权利。

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