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Exploration of underground structures with geophysical - seismic methods

机译:用地球物理 - 地震方法探索地下结构

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摘要

Seismic explorations are based on registration of seismic refraction and reflection of the elastic waves.In the processed geophysical data, obtained during the investigations of the archaeological site "Skupi", seismic explorations were conducted in combination of refraction and reflection. But, this paper presents the results only from refraction method.udDuring the research, the application of seismic methods is performed using measurement technique slalom by placing more geophones along the investigated area.udSlalom technique is based on registration of the generated elastic waves which spread through theudresearched area in the setted geophones.Using the moment of registration of elastic waves in audgeophone, by adjusting the time it can be assumed as a source of new elastic wave, which with furtherudregistration modeling the characteristics of the investigated terrain where it is placed.Through thisudtechnique with one generation of elastic waves are produced seismic models for each geophone, and for each subsequent decreases the depth of examination, because it cuts the measuring length of recording of the elastic waves.
机译:地震勘探是基于地震折射和弹性波反射的配准。在对“ Skupi”考古遗址进行调查的过程中获得的处理过的地球物理数据中,地震勘探是结合折射和反射进行的。但是,本文仅提供了折射法的结果。 ud在研究过程中,通过在被调查区域放置更多的检波器,使用测量技术回旋进行地震方法的应用。 udSlalom技术基于生成的弹性波的配准,借助设置在检波器中的弹性波的记录时刻,通过调整检波器中弹性波的记录矩,可以通过调整时间将其假定为新的弹性波的来源,并通过进一步的非注册来模拟地震波的特征。通过这种具有一代弹性波的技术,可以为每个地震检波器生成地震模型,并为每个随后的地震检波器减小了探测深度,因为它缩短了弹性波记录的测量长度。

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