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在苏联,近十年来,海岸地貌学的研究有了很大的发展,而对于海岸地带,即海与陆相互作用地带的泥砂运动及其迁移规律性的研究则是其中最重要的一个方向。实际上,正像所指出的,对岩石圈物质迁移过程的研究是从“岩石颗粒及原生岩塊的破碎开始直到它们在地质作用中重新结合为止”而且是作为研究地壳表面地形的形成及共发展的地貌学中的一个重要任务。正是在这个作用的过程中及其后果,就建立着并发展着各种地形的形态。通常,这些形态可划分为二种基本类型:剥蚀的和堆积的。
In the Soviet Union, the research on coastal geomorphology has progressed greatly in recent ten years, and the most important direction is the study of the movement of mud and sand and the migration regularity in the coastal zone, that is, the sea-land interaction zone. In fact, as it has been pointed out, the study of the lithosphere material migration process begins with the “fragmentation of rock particles and virgin rock blocks until they are reintegrated in geological processes” and as a means of studying the formation of the crustal surface topography An important task in the development of geomorphology. It is in the course of this role and its consequences that various forms of terrain have been established and developed. In general, these morphologies can be divided into two basic types: denuded and stacked.