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Landslides on the Eastern Slope of Sakhalin Island as Possible Tsunami Sources

机译:萨哈林岛东坡的滑坡可能是海啸的源头

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摘要

An underwater landslide located in the central part of the eastern slope of Sakhalin Island was found and mapped during investigations under the auspices of the Korean—Russian Project Sakhalin Slope Gas Hydrates (SSGH) [1, 2]. The study region was confined to a depression oriented in the northeasterly direction (Fig. la). The research in this region [1—4] demonstrated that closed depressions with round and slightly elongated forms in the northeasterly direction are characteristic peculiarities of the morphology of this depression (Fig. 1b).
机译:在韩俄项目萨哈林边坡天然气水合物(SSGH)的主持下进行的调查中,发现并绘制了位于萨哈林岛东坡中部的水下滑坡并绘制了地图[1,2]。研究区域仅限于向东北方向凹陷(图1a)。在该地区[1-4]的研究表明,在东北方向上呈圆形且略微拉长的闭合凹陷是该凹陷形态的特征(图1b)。

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  • 来源
    《Doklady Earth Sciences》 |2013年第1期|354-357|共4页
  • 作者单位

    Shirshov Institute of Oceanology, Russian Academy of Sciences, Nakhimovskii pr. 36, Moscow, 117997 Russia;

    Shirshov Institute of Oceanology, Russian Academy of Sciences, Nakhimovskii pr. 36, Moscow, 117997 Russia;

    Shirshov Institute of Oceanology, Russian Academy of Sciences, Nakhimovskii pr. 36, Moscow, 117997 Russia;

    Shirshov Institute of Oceanology, Russian Academy of Sciences, Nakhimovskii pr. 36, Moscow, 117997 Russia;

    Korean Polar Research Institute, Get-pearl Tower,Sondo Techo Par 12 Gaetbeol-ro, Yeonsu-gu, Incheon,406-840 Korea;

    Shirshov Institute of Oceanology, Russian Academy of Sciences, Nakhimovskii pr. 36, Moscow, 117997 Russia;

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