日本德岛岛户堆积复合体 1892 年暴雨事件引发的两次历史性深陷灾难性滑坡的地质和地貌原因

IF 1 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY
Island Arc Pub Date : 2024-11-26 DOI:10.1111/iar.70000
Noriyuki Arai
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引用次数: 0

摘要

1892 年,日本德岛县开府川上游在暴雨之后发生了灾难性的 Hose 和 Ogawatuetui 滑坡。该地区的地层为陡倾的相干地层,断层众多,位于岛户带,在暴雨和俯冲带大地震之后,该地区经常发生深层灾难性山体滑坡。滑坡发生的主要地质和地貌原因包括:局部地形起伏≥ 350 米(直径 1200 米的分析窗口);海拔 90-150 米处的节理点和斜坡断裂;上坡为具有开放性断裂的坚固块状厚层砂岩;下坡为高变形性和低渗透性的不坚固细砂岩和页岩薄层交替分布。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geological and Geomorphological Causes of Two Historical Deep-Seated Catastrophic Landslides Induced by the 1892 Heavy Rainfall Event in the Shimanto Accretionary Complex, Tokushima, Japan

The catastrophic Hose and Ogawatuetui landslides occurred coincidentally in 1892 following heavy rainfall in the upper reaches of the Kaifu River, Tokushima, Japan. The area is underlain by a steeply dipping coherent formation with many faults, and lies in the Shimanto Belt where deep-seated catastrophic landslides are known to occur following heavy rainfall and large subduction zone earthquakes. The main geological and geomorphological causes of the landslides were found to include local relief ≥ 350 m (1200-m-diameter analysis windows); knickpoints and slope breaks at 90–150 m above sea level, competent massive and thick-bedded sandstone with open fractures on the upper slope, and alternating thin beds of incompetent fine sandstone and shale beds of high deformability and low permeability on the lower slope.

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来源期刊
Island Arc
Island Arc 地学-地球科学综合
CiteScore
2.90
自引率
26.70%
发文量
32
审稿时长
>12 weeks
期刊介绍: Island Arc is the official journal of the Geological Society of Japan. This journal focuses on the structure, dynamics and evolution of convergent plate boundaries, including trenches, volcanic arcs, subducting plates, and both accretionary and collisional orogens in modern and ancient settings. The Journal also opens to other key geological processes and features of broad interest such as oceanic basins, mid-ocean ridges, hot spots, continental cratons, and their surfaces and roots. Papers that discuss the interaction between solid earth, atmosphere, and bodies of water are also welcome. Articles of immediate importance to other researchers, either by virtue of their new data, results or ideas are given priority publication. Island Arc publishes peer-reviewed articles and reviews. Original scientific articles, of a maximum length of 15 printed pages, are published promptly with a standard publication time from submission of 3 months. All articles are peer reviewed by at least two research experts in the field of the submitted paper.
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