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Titlebook: Submarine Mass Movements and Their Consequences; 6th International Sy Sebastian Krastel,Jan-Hinrich Behrmann,Carl Bonnev Book 2014 Springer

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發(fā)表于 2025-3-21 17:03:18 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Submarine Mass Movements and Their Consequences
副標題6th International Sy
編輯Sebastian Krastel,Jan-Hinrich Behrmann,Carl Bonnev
視頻videohttp://file.papertrans.cn/882/881337/881337.mp4
概述Unique subject that is addressed in very few other publications and interest is growing rapidly.State of knowledge of submarine mass movements and their consequences.Engineering and environmental cons
叢書名稱Advances in Natural and Technological Hazards Research
圖書封面Titlebook: Submarine Mass Movements and Their Consequences; 6th International Sy Sebastian Krastel,Jan-Hinrich Behrmann,Carl Bonnev Book 2014 Springer
描述Submarine mass movements are a hidden geohazard with large destructive potential for submarine installations and coastal areas. This hazard and associated risk is growing in proportion with increasing population of coastal urban agglomerations, industrial infrastructure, and coastal tourism. Also, the intensified use of the seafloor for natural resource production, and deep sea cables constitutes an increasing risk. Submarine slides may alter the coastline and bear a high tsunamogenic potential. There is a potential link of submarine mass wasting with climate change, as submarine landslides can uncover and release large amounts greenhouse gases, mainly methane, that are now stored in marine sediments.? .The factors that govern the stability of submarine slopes against failure, the processes that lead to slope collapses and the collapse processes by themselves need to be better understood in order to foresee and prepare society for potentially hazardous events. This book volume consists of a collection of cutting edge scientific research by international experts in the field, covering geological, geophysical, engineering and environmental aspects of submarine slope failures. The foc
出版日期Book 2014
關(guān)鍵詞Marine Hazards; Mass-movement; Submarine Landslide; Tsunamis
版次1
doihttps://doi.org/10.1007/978-3-319-00972-8
isbn_softcover978-3-319-37511-3
isbn_ebook978-3-319-00972-8Series ISSN 1878-9897 Series E-ISSN 2213-6959
issn_series 1878-9897
copyrightSpringer International Publishing Switzerland 2014
The information of publication is updating

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發(fā)表于 2025-3-21 22:09:52 | 只看該作者
Field Measurements to Investigate Submerged Slope Failuresliquefaction and breach flow. For these sites CPT’s and electrical resistivity cone tests available from earlier investigations, were extended with seismic CPT’s and interpreted for relative density and state parameter. The results of this study lead to the conclusion that some of the historical flo
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Evidence for Mass Transport Deposits at the IODP JFAST-Site in the Japan Trenchvered by a thin veneer of 50 cm hemipelagic, bioturbated diatomaceous mud. This stratigraphic boundary can be clearly distinguished by using physical properties data from Multi Sensor Core Logging and from fall-cone penetrometer shear strength measurements. The geochemical analysis of the pore-water
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Preliminary Investigations of Rheological Properties of Busan Clays and Possible Implications for DeBased on the relationship between the liquidity index and rheological values (viscosity and yield stress), flow motions are compared. Results show that the differences in mobility are significant when assuming that the flowing materials behave as a Bingham fluid. The runout distance is controlled by
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Utilizing Cone Penetration Tests for Landslide Evaluationnts such as shear resistance, probable slip surface and sensitivity of sediments. Liquefaction potential of sediments is assessed using vibratory CPT results. For dissipation tests, the cone remained stationary in the sediment for ~60 min to monitor pore pressure dissipation at the depths of 6, 9 an
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Post-failure Processes on the Continental Slope of the Central Nile Deep-Sea Fan: Interactions Betwes generate overpressures along the boundary between MTDs and overlying fine-grained sediment, resulting in a slow downslope movement of the sediment cover and formation of tilted blocks separated by faults. Fluids can migrate to the seafloor, leading to the construction of carbonate pavements. Where
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