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首页> 外文期刊>Geomorphology >Revisiting the slip rate of Quaternary faults in the Iberian Chain, NE Spain. Geomorphic and seismic-hazard implications
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Revisiting the slip rate of Quaternary faults in the Iberian Chain, NE Spain. Geomorphic and seismic-hazard implications

机译:重新审视伊伯利亚连锁店的第四纪断层的滑移率Ne西班牙。地貌和地震危害的影响

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The seismogenic potential of active faults for seismic hazard analyses are typically constrained using slip rates. These parameters, derived from numerically dated Quaternary deposits and landforms, have a critical impact on seismic hazard estimates with relevant societal and economic implications. Recently published geomorphological and paleoseismic investigations on active normal faults in the intraplate Iberian Chain (Spain), based on OSL ages from a now closed commercial laboratory, indicate anomalously high slip rates and paleoearthquake frequencies and extremely high fluvial incision rates. Parameters derived from those numerical ages have been used for seismic hazard assessments at critical facilities. This work revisits the chronology of Quaternary deposits associated with several faults applying various geochronological methods: Electro Spin Resonance (ESR), AMS Radiocarbon, Optically Stimulated Luminescence (OSL) and U-series dating. The totality of the new numerical ages is markedly different from the previously published OSL ages. The thirteen new ESR, OSL and U-series ages are systematically between three and six times older than the previous OSL ages. These data strongly suggest that previous ages overestimate the activity of the faults and seismic hazard in the region. The lack of validity of the revisited OSL analyses is attributed to inadequate dating procedures. Slip rates calculated with the new numerical ages are consistent with the slip rates estimated using Pliocene markers in the Iberian Chain and the slip rates published for other normal faults in eastern Spain. The new geochronological data also indicate reasonable fluvial incision rates, comparable with those estimated in nearby regions. The findings presented in this work have also implications for other Quaternary geomorphological studies in Spain based on potentially non-valid OSL ages. (C) 2020 Elsevier B.V. All rights reserved.
机译:地震危害分析的积极故障的发震潜力通常使用滑率约束。这些参数来自数值日期的第四纪沉积物和地貌,对具有相关社会和经济影响的地震危害估计产生了严重影响。最近公布了对Intrainal Inberian Chain(西班牙)的主动正常故障的地貌和古摆动调查,基于现在封闭的商业实验室的OSL年龄,表明异常高的滑动速率和古地震频率和极高的河流切口率。来自这些数值年龄的参数已用于关键设施的地震危害评估。这项工作重新评估与若干故障相关的第四纪矿床的年代学,应用各种地理学方法:电旋转共振(ESR),AMS RadioCarbon,光学刺激的发光(OSL)和U形序列约会。新数值年龄的整体与先前公布的OSL年龄明显不同。第十三个新ESR,OSL和U系列年龄系统地比以前的OSL年龄较大的三倍和六次。这些数据强烈表明,之前的年龄估计该地区的故障和地震危害的活动。 Repabited OSL分析的缺乏有效性归因于约会程序不充分。使用新数值年龄计算的滑移率与使用伊伯利亚链中的专业版标志物估计的滑移率以及在西班牙东部的其他正常断层公布的滑梯率。新的地理学数据还表明合理的河流切口率,与附近地区估计的人相当。本作品中提出的调查结果也基于潜在的无效OSL年龄对西班牙的其他第四纪地貌研究产生影响。 (c)2020 Elsevier B.v.保留所有权利。

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