提高为当地固体矿物预测和勘探而进行的地球物理调查结果解释可靠性的方法:地球动力学方法

N. Kasyanova
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引用次数: 0

摘要

背景。地球动力学方法在区域预测找矿工作中得到了有效的应用。然而,它在局部固体矿产预测和找矿中的应用是有限的,有时甚至是不可能的。局部矿产(固体、液体、气体)预测和找矿的关键问题之一是非标准(闪烁)物探异常的存在,这给地质勘探不同阶段、不同时间进行的物探结果解释带来了困难。本文在研究现代地球动力学过程发展的时空格局及其对地球物理场影响的基础上,阐述了利用地球动力学研究进行局部固体矿产预测和找矿的可能性。的目标。提高为当地固体矿物预测和勘探而进行的地球物理调查结果解释的可靠性。材料和方法。本研究是在综合分析文献资料、基金资料和本人在现代地球动力学和找矿勘探地球动力学领域多年研究成果的基础上进行的。最初的数据是基于各种地球物理场(变形、地震和地表磁)的监测数据。建立了地球地球物理场(特别是磁场)中闪烁异常出现的地球动力学原因,并提出了它们在现代地球动力学过程影响下形成的机制。扩大了地球动力学方法在固体矿产找矿中的应用可能性,提出了提高局部找矿效率的方法。这项研究表明,有可能利用地球动力学研究在当地寻找固体矿物,这有助于提高地球物理调查数据解释结果的可靠性,从而减少寻找矿藏所涉及的总的财政和时间费用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Ways to improve the reliability of interpreting the results of geophysical surveys performed for the local forecast and prospecting for solid minerals: a geodynamic approach
Background. The geodynamic approach is effectively used in regional forecasting and prospecting works. However, its application for local forecasting and prospecting for solid minerals is limited and sometimes impossible. One of the key problems of local forecasting and prospecting for minerals (solid, liquid, gaseous) is the presence of non-standard (flickering) geophysical anomalies, which complicates the interpretation of the results of geophysical surveys performed at different times at different stages of geological exploration. The article is devoted to clarifying the possibility of using geodynamic research in local forecasting and prospecting for solid minerals on the basis of attracting the latest scientific knowledge from the field of studying the spatio-temporal patterns of the development of modern geodynamic processes and their influence on the Earth’s geophysical fields. Aim. To increase the reliability of interpreting the results of geophysical surveys performed for local forecasting and prospecting for solid minerals.Materials and methods. The research was carried out on the basis of a comprehensive analysis of literature data, fund materials and the results of many years of the author’s own research in the fields of modern geodynamics and prospecting and exploration geodynamics. The initial data were based on the monitoring data of various Earth’s geophysical fields (deformation, seismic, and surface magnetic).Results. A geodynamic reason for the appearance of flickering anomalies in the Earth’s geophysical fields (in particular, magnetic) has been established, and a mechanism for their formation under the influence of modern geodynamic processes has been proposed. The possibility of using the geodynamic approach in the prospecting for solid minerals has been expanded, and ways to increasing the efficiency of local searches have been proposed.Conclusions. The research demonstrates the possibility of using geodynamic studies in local prospecting for solid minerals, which helps to increase the reliability of the results of interpretation of geophysical survey data, and, as a result, to reduce the overall financial and time costs involved with searching for mineral deposits.
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