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Volcaniclastic tide-modulated tempestite in a coastal tuff ring Jeju Island Korea

机译:韩国济州岛沿海凝灰岩环中的火山碎屑潮汐调制的白云母

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摘要

The need for more accurate and extensive records of storm activity is increasing because of growing population and infrastructure in coastal areas. Records of past storm activity have consequently been sought from diverse sedimentary proxies in marginal marine environments, as well as historical documents. In this paper, we introduce a unique record of a 3.7 ka BP storm event preserved in a coastal tuff ring on Jeju Island, Korea. The tuff ring formed mostly above high tide level by primary volcanic processes, but contains three interbeds of horizontally laminated to hummocky/swaly cross-stratified deposits with intervening mud drapes up to an altitude of ~4.6 m above high tide level. These interbeds were formed by wave activity in a swash to surf zone when the sea level rose several meters above normal high-tide level during a storm event, and the triple intercalation of the wave-worked deposits reflects three tidal cycles during a storm event that lasted 1.5 day. Jeju Island contains the most complete record of an ancient storm event ever reported in the tuff ring, and highlights the significance of coastal volcanoes in the study of extreme depositional events in coastal areas, such as storms and tsunamis.
机译:由于沿海地区人口和基础设施的增加,对风暴活动更准确和广泛记录的需求日益增长。因此,已经从边缘海洋环境中的各种沉积物代理人以及历史文献中寻找过往风暴活动的记录。在本文中,我们介绍了保存在韩国济州岛沿海凝灰岩环上的一次3.7 ka BP风暴事件的独特记录。凝灰岩环主要是通过一次火山作用在高潮位以上形成的,但包含三个水平夹层,中间夹杂着垂向/倾斜的交叉分层的沉积物,中间的泥垂到高潮位以上约4.6μm。这些夹层是由风暴活动期间海平面上升到比正常高潮水位高出几米的斜波冲浪区的波浪活动形成的,波浪作用沉积物的三层夹层反映了风暴事件期间的三个潮汐周期。持续了1.5天。济州岛包含有史以来在凝灰岩环中报告的最完整的古代风暴事件记录,并突显了沿海火山在研究风暴和海啸等沿海地区极端沉积事件中的重要性。

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