Titlebook: Marine Slides and Other Mass Movements; Svend Saxov,J. K. Nieuwenhuis Book 1982 Plenum Press, New York 1982 Coast.Ocean.Oceanography.marin

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书目名称Marine Slides and Other Mass Movements影响因子(影响力)




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书目名称Marine Slides and Other Mass Movements网络公开度学科排名




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书目名称Marine Slides and Other Mass Movements被引频次学科排名




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Adornment

On the Tectonic Setting of Submarine Slidesnic” agents, such as deposition, toe-erosion and pore pressure conditions. This is inferred from the existence of a principle of correspondence between subaerial and subaqueous phenomena based on the notion of effective pressure. Inasmuch as it can be shown that subaerial slides are co-determined by

Counteract

HAUNT

miracle

MEET

Submarine Slumping and Mass Movements on the Continental Slope of Israel Lebanon. The lens was formed by accumulation, since the Pliocene time, of mainly fine clastics derived from the Nile and transported by the counterclockwise currents of the south-eastern Mediterranean. After initial deposition, the detritus was redistributed over the continental slope and the adjac

ornithology

向外才掩饰

Marine Slope Stability — A Geological Approaching this volume. On the other hand, basic information available to geoscientists on how marine slides or slope instability can be investigated is widely scattered. This paper attempts to fill the gap by briefly discussing mthods for preliminary surveys, sampling, and analysis. Emphasis is placed on

索赔

Imaging of Submarine Landslides with Wide-Swath Sonarantic. Their detection and mapping has been accomplished with a tethered deep-ocean side-scan sonar having a swath width of 5 km. The sonar was constructed to search for and locate the wreck of the S. S. TITANIC (Wilford, 1980). We have subsequently used it in cooperation with the U.S. Geological Su

使人入神

Anatomy of Some Atlantic Margin Sediment Slides and Some Comments on Ages and Mechanisms of a 18,000 km. slide scar with a 30,000 km. area of slide deposits. The total displaced volume is of the order of 1100 km.. The scar is bounded on its eastern and southern sides by 10 to 100 m scarps. The failure occurred over a slope of about 1° to 1.5° and the mass flows moved over slopes as gen