...
首页> 外文期刊>Geografiska Annaler, Series A. Physical Geography >High-precision Schmidt-hammer exposure-age dating of flood berms, Vetlest?lsdalen, alpine southern Norway: First application and some methodological issues
【24h】

High-precision Schmidt-hammer exposure-age dating of flood berms, Vetlest?lsdalen, alpine southern Norway: First application and some methodological issues

机译:挪威南部阿尔卑斯山脉Vetlest?lsdalen洪水堤的高精度施密特锤暴击年龄测定:首次应用和一些方法学问题

获取原文
获取原文并翻译 | 示例
           

摘要

Schmidt-hammer exposure-age dating (SHD) was applied to three flood berms in upper Vetlest?lsdalen, southern Norway, using a local, high-precision calibration curve that takes account of the colluvial origin of fluvial boulders in the youngest berm, which was deposited during the August 1979 flood. Precision of SHD dating for this berm was estimated as ±210 years, whereas predicted ages of the two older berms were 3195±435 and 3405±340 years, and subsections of the oldest berm yielded age ranges of ~900 years. The results demonstrate the feasibility of high-precision SHD in the context of boulder landforms deposited by high-magnitude floods, the requirement of a large sample of R values in the face of high natural variability, the necessity of an appropriate calibration curve to ensure accuracy, the usefulness of floods of known age for testing and improving calibration curves, and the potential effects of boulders of colluvial origin on R values (especially the susceptibility of young surfaces to roughness variations). The dated berms indicate a return period of ~1000-1500 years for floods of the magnitude of the 1979 flood event in the upper catchment. Thus, the long-term persistence of flood boulder berms in the landscape has potential for reconstructing Holocene flood history and palaeohydrology from the geomorphic legacy of the most extreme Holocene floods.
机译:施密特-锤击暴露年龄测年(SHD)被应用到挪威南部上韦特尔斯特斯代尔嫩的三个洪泛河道,采用局部高精度校准曲线,该曲线考虑了最年轻河道中河流卵石的河流成因。是在1979年8月的洪水期间沉积的。该病的SHD测年精度估计为±210年,而两个较早的病床的预测年龄为3195±435和3405±340岁,最古老的病床的各个分部的年龄范围为〜900年。结果表明,在高强度洪水沉积的巨石地貌的情况下,高精度SHD的可行性,面对高自然变异性需要大量R值样本,需要使用适当的校准曲线以确保准确性的必要性,已知年龄的洪水对测试和改善标定曲线的有用性,以及洞穴起源的巨石对R值的潜在影响(尤其是年轻表面对粗糙度变化的敏感性)。标有日期的护堤表明上游流域1979年洪水事件的洪水重现期约为1000-1500年。因此,洪水巨石护堤在景观中的长期存在可能从最极端的全新世洪水的地貌遗产中重建全新世的洪水历史和古水文学。

著录项

相似文献

  • 外文文献
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号