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Method of Non Destructive Geophysical Mapping of the Environment

机译:环境的非破坏性地球物理测绘方法

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Problem statement: The method of non-destructive testing is needed in different aspects of geology, geomechanics and archeology, for instance: by testing the state of rock massifs in sault, kimberlites or rock shock mines, ancient archeological objects, or mapping for locating the wells drilling. The best method for solution these problems is based on using induction multi frequency electromagnetic field with use control sources on 3D planshet system of observation. Applied methods and design: Such method was developed at the Institute of Geophysics, Ural Branch of the Russian Academy of Sciences that allows its use to solve complex geological problems for mapping and monitoring the state of the environment. Its use allows the observation system to be used in such way that, on the one hand, it achieves flexible tunable detail of observations, and on the other hand, it organizes an input database that is close to the domain of definition of the inverse problem operator in the class of layered-block models with local hierarchical inclusions. This allows using regularization methods to obtain solutions that are in the class of equivalent, close to true. The specific possibilities of its use are determined by the technical side: the power of the excitation source, the sensitivity of the receiving system. Typical results: It had been developed a new method of mapping, processing and interpretation, realized in a set of programs that allow seeing the result of the searching structure of the environment in real time (that is after receiving some results during one day, we can see the results of the geoelectrical features of the structure and the state of that part of the environment). It had been suggested a three staged conception of interpretation that can be used not only for interpretation electromagnetic induction data and dynamic seismic data. Concluding note (Practical value/implications): In the considered case, this method contributed to the study of altered forms of kimberlitic bodies. The method underwent geological verification in various geological conditions where it had been used for mapping the geoelectrical structure. This allows us to offer a method for the development of innovative technology in the search for hydrocarbons in complex geological structures. The method was used in Egypt for research ancient archeological objects, located in Alexandria.
机译:问题陈述:在地质,地质力学和考古学的各个方面都需要采用非破坏性测试的方法,例如:通过测试底坑,金伯利岩或岩石冲击波地雷的岩石断层的状态,古代考古对象或用于定位矿床的地图钻井。解决这些问题的最佳方法是基于在3D平面观测系统上使用感应多频电磁场和控制源。应用的方法和设计:这种方法是由俄罗斯科学院乌拉尔分校地球物理研究所开发的,可用于解决复杂的地质问题,以绘制地图和监测环境状况。它的使用允许以这样的方式使用观测系统:一方面,它可以实现灵活的观测细节可调,另一方面,它可以组织一个与反问题的定义域接近的输入数据库。局部分层包含的分层块模型类中的算子。这允许使用正则化方法来获得等效类中的近似真实的解。其使用的具体可能性由技术方面确定:激发源的功率,接收系统的灵敏度。典型结果:已经开发了一种新的映射,处理和解释方法,并通过一组程序实现,这些程序可以实时查看环境搜索结构的结果(也就是说,在一天中收到一些结果之后,可以看到结构的地电特征结果以及该部分环境的状态)。已经提出了解释的三个阶段的概念,其不仅可以用于解释电磁感应数据和动态地震数据。结论(实用价值/含义):在考虑的情况下,该方法有助于研究金伯利岩体的变化形式。该方法在各种地质条件下进行了地质验证,并已被用于绘制地电结构图。这使我们能够提供一种开发创新技术的方法,以寻找复杂地质结构中的碳氢化合物。该方法在埃及用于研究位于亚历山大的古代考古对象。

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