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

TINGE

书目名称Submarine Mass Movements and Their Consequences影响因子(影响力)




书目名称Submarine Mass Movements and Their Consequences影响因子(影响力)学科排名




书目名称Submarine Mass Movements and Their Consequences网络公开度




书目名称Submarine Mass Movements and Their Consequences网络公开度学科排名




书目名称Submarine Mass Movements and Their Consequences被引频次




书目名称Submarine Mass Movements and Their Consequences被引频次学科排名




书目名称Submarine Mass Movements and Their Consequences年度引用




书目名称Submarine Mass Movements and Their Consequences年度引用学科排名




书目名称Submarine Mass Movements and Their Consequences读者反馈




书目名称Submarine Mass Movements and Their Consequences读者反馈学科排名

繁荣中国

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

dialect

使出神

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

Corroborate

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

installment

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

背景

平项山

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

aqueduct

轻推