Titlebook: Submarine Mass Movements and Their Consequences; 3rd International Sy Vasilis Lykousis,Dimitris Sakellariou,Jacques Loca Book 2007 Springer

遺傳學(xué)

Flood-Induced Turbidites From Northern Hudson Bay And Western Hudson Strait: A Two-Pulse Record Of Liz into the North Atlantic around 8500 cal BP. It has been suggested that this catastrophic event may have triggered the 8200 cal BP cold event recorded in Greenland ice cores. Evidence for that outburst flood was the identification of a centimeter to decimeter-thick hematiterich red layer that was

冥界三河

政府

Anthropogenic Turbidity Current Deposits In A Seismically Active Graben, The Gulf Of Corinth, Greeced dispersion of bauxitic “red mud” tailings. The red mud tailings have been discharged at a rate of 500 000 to 640 000 tonnes/year via submerged outfalls on the shelf at a water depth of 100 m. The red mud tailings at the mouth of the outfalls have formed three oval shaped mounds. These mounds have

愛(ài)花花兒憤怒

象形文字

The Southern Flank Of The Storegga Slide: Imaging And Geomorphological Analyses Using 3d Seismicossible to identify another compression zone. A relative chronology of events was established and it is proposed that these two compressions zones are the result of gravity-driven slope failures related to different stages of the Holocene Storegga Slide.

grotto

Submarine Mass Movements On An Active Fault System In The Central Gulf Of Corinthme of them are fault controlled. The head and the walls of the canyons are affected by mass failures. It is estimated that about 1.1 km3 of mass failed sediments have been removed from the canyons and transported downslope to the basin floor.

dysphagia

FOLD

Submarine Paleo-Failure Morphology On A Glaciated Continental Margin From 3d Seismic Datanstable sediments extends beyond the paleo-slide scar. The upper surface morphology is dominated by three straight to slightly meandering paleo-channels, at least one of them formed by mass wasting. Together, the two paleo-surfaces exemplify slope morphology that may result from sediment instability on glaciated margins.

LIMN

Landslide And Gravity Flow Features And Processes Of The Nazaré And Setúbal Canyons, West Iberian Masupply to canyon heads, and thicker, siliciclastic coarse sandy turbidites, probably generated by larger earthquake-triggered slope failures on much longer timescales. Our results highlight the complex interplay of sedimentary processes operating within major canyon systems.

土坯

1878-9897 infrastructures but also for the exploitation and the development of seafloor resources. A tragic example of the vulnerability of coastal communities has been provided by the Indonesian tsunami of December 2004. Since 2005, as part of the scientific community efforts to minimize the impact of such n