库页岛东北部泻湖海峡的形态岩石动力学

Q4 Earth and Planetary Sciences
V. V. Afanasev, Владимир Владимирович Афанасьев
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引用次数: 0

摘要

介绍了萨哈林东北部泻湖海岸结构和动力学的地理空间和地质信息分析结果。基于1927年至2014年期间泻湖海峡海岸侵蚀累积过程和迁移的一些参数。考虑了萨哈林东北部的地貌动力学系统。海峡迁移过程中运输的沉积物体积是在三维模型的帮助下估计的,在三维模型中,与时间平均的侵蚀和堆积区域平行,使用了额外的数据,即:海峡和邻近水域的水深测量,屏障形式的起伏特征以及通过地质雷达测量和钻探获得的地质信息。地质雷达数据加上遥感数据,使建立沉积模型成为可能,这为分析观测期后海岸形成的历史奠定了基础。目前,我们可以将这种情况追溯到19世纪中叶。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Morpholithodynamics of lagoonal straits of the North-Eastern Sakhalin
The results of the analysis of geospatial and geological information on the structure and dynamics of the lagoon coast of the North-Eastern Sakhalin are presented. On the basis of a number of parameters of the coastal erosion-accumulation processes and migration of lagoon straits during the period 1927–2014. the morpholithodynamics system of the North-Eastern Sakhalin was considered. The volume of sediments transported during the migration of the straits, was estimated with the help of three-dimensional models, in which, parallel with time-averaged areas of erosion and accumulation, additional data were used, namely: bathymetry of the straits and adjacent water area, characteristics of the relief of the barrier forms and geological information obtained as a result of georadar survey and drilling. Georadar data, together with remote sensing data, have made it possible to create a model of sedimentation, which formed the basis for the analysis of the history of the coast formation beyond the period of observations. Currently, we can trace the situation as long as to the middle of the XIXth century.
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来源期刊
Geomorfologiya
Geomorfologiya Earth and Planetary Sciences-Earth-Surface Processes
CiteScore
0.80
自引率
0.00%
发文量
8
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