outset
发表于 2025-3-27 00:37:40
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富足女人
发表于 2025-3-27 01:36:36
Along Slope Variations In Mass Failures And Relationships To Major Plio-Pleistocene Morphological Elflection and multibeam bathymetry data provide a better understanding of mass failure processes. A semicontinuous seismic section along the upper slope from Flemish Pass to north of Hamilton Spur shows an alternation of major morphological elements that includes canyons and failure corridors, inter-
割让
发表于 2025-3-27 08:24:56
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真实的人
发表于 2025-3-27 10:32:57
The Southern Flank Of The Storegga Slide: Imaging And Geomorphological Analyses Using 3d Seismicplexity it is far from being fully understood. Three-dimensional (3D) seismic combined with swath bathymetry data from the southern flank of the Storegga Slide have been used to study mass movement processes occurring in the region. The high spatial resolution provided by the 3D seismic data has all
空气传播
发表于 2025-3-27 16:09:02
Submarine Mass Movements On An Active Fault System In The Central Gulf Of Corinthled that three morphological zones characterize the area: the shelf, the slope and the basin. Three E-W trending, right stepping basin bounding faults define the basin-slope contact, producing a step like configuration along the base of slope. Steep scarps, caused by mass failures, sculpt the fault
Fissure
发表于 2025-3-27 20:22:42
Analysis Of Multibeam Seafloor Imagery Of The Laurentian Fan And The 1929 Grand Banks Landslide Areae-triggered tsunami and turbidity current. The event is well constrained in terms of trigger, timing, sequence of events and impact. The landslide site was surveyed in September of 2006 with a 12 kHz multibeam echosounder. Regionally, these bathymetric data show canyons, valleys and gullies, somewha
temperate
发表于 2025-3-27 23:21:40
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Radiation
发表于 2025-3-28 04:23:43
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amyloid
发表于 2025-3-28 06:15:03
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Endemic
发表于 2025-3-28 13:25:14
Submarine Spreading: Dynamics And Developmentr, recent advances in seafloor imaging techniques show that repetitive extensional patterns of parallel ridges and troughs, oriented perpendicular to the direction of mass movement and typical of spreading, are widespread offshore. A spread develops via the failure of a surficial sediment unit into