Titlebook: Offshore Tidal Sands; Processes and deposi A. H. Stride Book 1982 Chapman and Hall Ltd 1982 Coast.Sediment.Sedimentation.evolution.growth.i

Stricture

Optimum

惊奇

Offbeat

hand, the discussions have blurred the parts played by the people concerned. This applies to all chapters in varying degrees, but is especially true for Chapters 3, 4 and 5. The authorship attributed to each chapter therefore seeks to reflect those who were most con­ cerned with it.978-94-009-5728-2978-94-009-5726-8

争论

绝缘

Tidal currents of the continental shelf,coast of the British Isles, are dominated by tides. Even in areas of small tidal range strong local tidal currents can occur, either near to a ‘node’ in a stationary tidal oscillation (Section 2.3) or because of bathymetry, particularly in channels or straits connecting two regions — for instance the Strait of Messina in the Mediterranean.

宽容

confederacy

赞美者

Offshore tidal deposits: sand sheet and sand bank facies,sive than sands or gravels because of the large areas of continental shelf with relatively weak tidal currents. However, as shown below, mud deposits are much less of an indicator of tidal current sedimentation than the sands and gravels, and will not be treated in detail.

破裂

Book 1982ntinental shelves. This task was initiated because of the need to define the next phase of research in this field by the Marine Geology Group of the Institute of Oceano­ graphic Sciences. Related indications of the longer term evolution of the deposits were sought by close reference to the nature of