非均质层状底构造地质模型的形成原理

O. I. Shundel, S. Fedoseienkov, S. Nevierova
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引用次数: 0

摘要

本文介绍了具有简单和复杂形状空腔的层状地质构造的分析和数值模拟方法的发展和实现。发展了作者对海洋沉积物声学特性的结构和空间分布进行数学建模的分析和数值方法,将其作为层状非均匀介质,允许创建考虑分层,各种形状和性质的空腔和包裹体的存在的非均匀海床的离散,连续或混合结构-声学模型。根据这些算法实现的地质分层环境模型,对于全景测量(SSS)建模、干涉通道SSS建模、多波束测深、三维剖面、基于测深测量的等深图绘制等都是必要的。
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PRINCIPLES OF FORMATION OF STRUCTURAL GEOLOGICAL MODELS OF HETEROGENEOUS LAYERED BOTTOM
The article describes the developed and implemented analytical and numerical methods for modeling layered geological structures with cavities of simple and complex shape. The developed author’s analytical and numerical methods of mathematical modeling of the structure and spatial distribution of acoustic properties of marine sediments, presented as a layered inhomogeneous medium, which allow to create discrete, continuous or mixed structural-acoustic models of inhomogeneous seabed taking into account stratification, the presence of cavities and inclusions of various shapes and properties. Models of geological layered environment implemented according to these algorithms are necessary for modeling panoramic survey (SSS), SSS with interferometric channel, multibeam sounder, three-dimensional profiling, construction of isobathic maps based on sounder measurements.
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发文量
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审稿时长
6 weeks
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