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The sedimentary and geomorphological imprint of the AD 365 tsunami on the coasts of southwestern Crete (Greece) - Examples from Sougia and Palaiochora

机译:克里特岛西南部(希腊)沿海地区公元365年海啸的沉积和地貌印记-以Sougia和Palaiochora为例

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摘要

The southwestern coast of Crete, one of the most seismically active regions in Europe, experienced co-seismic crust uplift by 9 m during the Ms = 8.3 mega-earthquake that struck the eastern Mediterranean world on 21 July AD 365. An associated tsunami event caused thousands of fatalities and destroyed many coastal settlements and infrastructure between the Levante in the east and the Adriatic Sea in the northwest. So far, coastal sedimentary archives in southwestern Crete including distinct palaeotsunami fingerprints are rarely investigated. Therefore, a multi-proxy study including sedimentological, geochemical, geochronological, and microfaunal methods was conducted in order to detect onshore coastal sedimentary archives that functioned as fine sediment traps and document palaeotsunami imprint. We found adequate archives at the Sougia and Palaiochora coastal plains that were used to reconstruct the palaeogeographical evolution and the palaeoseismological history of SW Crete during the late Holocene. Our studies revealed distinct geomorphological, sedimentological, geochemical, and microfaunal traces of high-energy impact from the marine side related to seismic events. At the Sougia coastal plain a sheet of fine sand with a neat microfossil and geochemical fingerprint was found sandwiched between underlying pre-tsunami muds and overlying post-tsunami colluvial silt. In the Palaiochora coastal plain, tsunami overflow of a flat Neogene bedrock platform led to the accumulation of sand-dominated deposits that were subsequently covered by colluvial material from the adjacent hill-slopes. Based on radiocarbon and luminescence dating approaches, it is shown that the AD 365 tsunami event is the best-fit candidate for the tsunami-related sediments deposited at both, Sougia and Palaiochora. This study, for the first time, presents multi-proxy evidence of the AD 365 tsunami imprint on fine-sedimentary archives along the western and southwestern coast of Crete. (C) 2017 Elsevier Ltd and INQUA. All rights reserved.
机译:克里特岛西南海岸是欧洲地震最活跃的地区之一,在公元365年7月21日袭击东地中海世界的Ms = 8.3特大地震中,同震地壳抬升9 m。与之相关的海啸事件引起了东部的莱万特(Levante)与西北的亚得里亚海(Adriatic Sea)之间的成千上万人丧生,并摧毁了许多沿海定居点和基础设施。到目前为止,很少对克里特岛西南部的沿海沉积档案库进行过研究,包括不同的古海啸指纹。因此,进行了一项包括沉积学,地球化学,地质年代学和微动物学方法在内的多代理研究,以检测起精细沉积物陷阱作用并记录古海啸印记的近岸沿海沉积档案。我们在Sougia和Palaiochora沿海平原发现了足够的档案,这些档案用于重建全新世晚期西南克里特岛的古地理演化和古地震学历史。我们的研究揭示了与地震事件有关的来自海洋一侧的高能影响的明显地貌,沉积学,地球化学和微真菌痕迹。在Sougia沿海平原上,发现一块细沙,上面带有微化石和地球化学指纹,夹在下面的海啸前泥浆和上覆的海啸后泥沙之间。在Palaiochora沿海平原,平坦的Neogene基岩平台的海啸溢流导致了以砂为主的沉积物的堆积,这些沉积物随后被相邻山坡上的冲积物质覆盖。基于放射性碳和发光测年方法,表明AD 365海啸事件是在Sougia和Palaiochora沉积的海啸相关沉积物的最佳候选者。这项研究首次提供了克里特岛西部和西南沿岸精细沉积档案中AD 365海啸烙印的多重代理证据。 (C)2017爱思唯尔有限公司和INQUA。版权所有。

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  • 来源
    《Quaternary International》 |2018年第ptaa期|66-90|共25页
  • 作者单位

    Johannes Gutenberg Univ Mainz, Inst Geog Nat Hazard Res & Geoarchaeol, Johann Joachim Becher Weg 21, D-55099 Mainz, Germany;

    Aix Marseille Univ, Ctr Camille Jullian, CNRS, UMR 7299,MMSH, 5 Rue Chateau Horloge, F-13090 Aix En Provence, France;

    Johannes Gutenberg Univ Mainz, Inst Geog Nat Hazard Res & Geoarchaeol, Johann Joachim Becher Weg 21, D-55099 Mainz, Germany;

    Johannes Gutenberg Univ Mainz, Inst Geog Nat Hazard Res & Geoarchaeol, Johann Joachim Becher Weg 21, D-55099 Mainz, Germany;

    Johannes Gutenberg Univ Mainz, Inst Geog Nat Hazard Res & Geoarchaeol, Johann Joachim Becher Weg 21, D-55099 Mainz, Germany;

    Johannes Gutenberg Univ Mainz, Inst Geog Nat Hazard Res & Geoarchaeol, Johann Joachim Becher Weg 21, D-55099 Mainz, Germany;

    Hellen Minist Culture, Ephorate Antiqu Rethymnon, Rethimnon 74100, Crete, Greece;

    Hellen Minist Culture, Ephorate Antiqu Chania, 4th Floor, Khania 73134, Crete, Greece;

    Rheinisch Westfalische Tech Univ Aachen, Neotecton & Nat Hazard Res Grp, Lochnerstr 4-20, D-52056 Aachen, Germany;

    Agr Univ Athens, Dept Nat Resources Dev & Agr Engn, Mineral Geol Lab, 75 Iera Odos St, GR-11855 Athens, Greece;

    Johannes Gutenberg Univ Mainz, Inst Geog Nat Hazard Res & Geoarchaeol, Johann Joachim Becher Weg 21, D-55099 Mainz, Germany;

    Johannes Gutenberg Univ Mainz, Inst Geog Nat Hazard Res & Geoarchaeol, Johann Joachim Becher Weg 21, D-55099 Mainz, Germany;

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  • 入库时间 2022-08-18 03:35:08

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