应用地球物理方法解决海洋和大湖泊地质生态学中的广泛问题

A. Rybalko, M. Tokarev, Y. Terekhina, A. Loktev, S. Mironyuk, A. Roslyakov, V. Shcherbakov, A. Kolyubakin
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引用次数: 0

摘要

地球物理方法近年来越来越多地用于地质生态学研究,包括工程和地质调查以及陆架底土的状态监测。应用最广泛的是各种类型的地震声剖面、侧扫声纳、多波束回声测深。地震声学方法提供了地质体形态的概念,并间接指示了它们的成因和包围沉积物的组成。它们最广泛地用于气体沉积物的评估和重力过程的识别。侧扫声纳可以识别冰冲刷区域,给出地形中形态的尺寸,以及估计岩石动力流动的强度、类型和方向。多波束回声测深使人们能够评估大面积海床的形态,并根据其数量特征区分各种成因类型的地形。该报告提供了许多使用地球物理方法解决各种地质生态问题的例子。结论是,对于确定冻结岩石的厚度和分布等任务,目前阶段的地球物理方法还不能给出明确的答案。指出有必要编写一份关于使用地球物理方法解决地质生态问题的方法手册。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Use of Geophysical Methods for Solving a Wide Range of Problems in The Geoecology of Seas and Large Lakes
Summary Geophysical methods have recently been increasingly used in geoecological studies, including engineering and geological surveys and state monitoring of the shelf subsoil. The most widely used are various types of seismoacoustic profiling, side-scan sonar, multi-beam echo sounding. Seismoacoustic methods give an idea of the morphology of geological bodies and indirectly indicate their genesis and composition of the enclosing sediments. They are most widely used in the assessment of gaseous sediments and in the identification of gravitational processes. Side-scan sonar makes it possible to identify zones of ice scouring, to give the dimensions of relief mesoforms, as well as to estimate the intensity, type and direction of lithodynamic flows. Multi-beam echo sounding allows one to assess the morphlology of the seabed over large areas and to distinguish various genetic types of relief with their quantitative characteristics. The report provides numerous examples of the use of geophysical methods for solving various geoecological problems. It is concluded that for tasks such as determining the thickness and distribution of frozen rocks, geophysical methods at the present stage cannot give an unambiguous answer. The need to prepare a methodological manual on the use of geophysical methods for solving geoecological problems is indicated.
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