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首页> 外文期刊>Sedimentary geology >Nine unusually large tsunami deposits from the past 4000 years at Kiritappu marsh along the southern Kuril Trench
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Nine unusually large tsunami deposits from the past 4000 years at Kiritappu marsh along the southern Kuril Trench

机译:在过去的4000年中,沿着千岛海沟南部的Kiritappu沼泽中有9个异常大的海啸沉积物

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摘要

Large earthquakes along the Kuril subduction zone in northern Japan are known to have caused damaging tsunami, although there is a little information on historical earthquakes and tsunami in this area because no documents exist before the 19th century that might refer to tsunami events. To determine the likely timing and size of future events we need information on their recurrence intervals and to do this for the prehistoric past we have investigated sediments located in the Kiritappu marsh in eastern Hokaido that we interpret as laid down by tsunami. Using reliable multiple lines of evidence from sedimentological, geomorphological, micropaleontological, and chronological results, we identify 13 tsunami sands. Two of these lie within a peat bed above a historical tephra, Ta-a (AD 1739); the upper one probably corresponds to the AD 1843 Tempo Tokachi-oki earthquake (A/8.2) tsunami, and the lower to either the AD 1952 Tokachi-oki earthquake (M 8.2) tsunami or the AD 1960 Chilean earthquake (M 9.5) tsunami. Underlying are 11 prehistoric tsunami sand beds (nine large sand beds and two smaller sand beds) deposited during the past 4000 years. Because of the wide spatial distribution of the large sand beds, and inundation distances inland of between 1200 to 3000 m, we suggest that they record unusually large tsunamis along the Kuril subduction zone. According to our analyses, these tsunami sands were derived from the coastal area and, although they do not show clear graded bedding, they commonly have gradational upper boundaries and erosional bases and include internal sedimentary structures such as plane beds, dunes, and current ripples, reflecting bedload transportation. Based on our results we calculate the recurrence interval of unusually large earthquakes (probably M 8.6) along the Kuril subduction zone as about 365-553 years and estimate the youngest large event to have occurred in the 17th century.
机译:众所周知,日本北部千岛俯冲带沿岸的大地震造成了破坏性的海啸,尽管有关该地区历史地震和海啸的信息很少,因为在19世纪之前还没有任何有关海啸事件的文献。为了确定未来事件的可能发生的时间和规模,我们需要有关其复发间隔的信息,并针对史前历史进行调查,我们调查了北海道东部基里塔普沼泽沉积物,我们将其解释为海啸造成的沉积物。利用来自沉积学,地貌学,微古生物学和年代学结果的可靠的多条证据,我们确定了13种海啸沙土。其中两个躺在历史悠久的特非拉塔阿(Ta-a,公元1739年)上方的泥炭床上。较高的可能对应于公元1843年的十日冲木(A / 8.2)海啸,而较低的对应于1952年的十胜木(M 8.2)海啸或1960年智利的地震(M 9.5)海啸。在过去的4000年中,沉积了11个史前海啸沙床(九个大沙床和两个小沙床)。由于大沙床的空间分布广泛,内陆的淹没距离在1200至3000 m之间,我们建议他们在千岛俯冲带记录到异常大的海啸。根据我们的分析,这些海啸沙粒来自沿海地区,尽管它们没有显示清晰的渐变层理,但它们通常具有渐变的上界和侵蚀基础,并且包括内部沉积结构,例如平面床,沙丘和潮流波纹,反映床载运输。根据我们的结果,我们计算出沿千岛俯冲带异常大的地震(可能是M 8.6)的复发间隔约为365-553年,并估计了17世纪最年轻的大地震发生了。

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