Berovo附近Bela Voda地区的地震勘探

Q4 Earth and Planetary Sciences Geologica Macedonica Pub Date : 2020-01-01 DOI:10.46763/geol20020111d
Blagica Doneva
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引用次数: 0

摘要

本文介绍了在Berovo附近的村庄Dvorište Bela Voda进行的勘探结果。现场调查的目的是根据所代表的构造构造和水文地质结构,确定地下水的供水潜力,根据指示的地下水捕获潜力、条件和机会,定位和预测设计供水探井。由于地球物理测量的需要,以前曾对该地形进行过野外水文地质勘察。对研究区内的地形水文地质特征和含水环境类型进行了界定和说明的地点,进行了水文地质研究和地球物理测量。通过代表性的调查剖面和对已知地质资料的分析,对地形上的构造-构造组合进行了反射地震扫描。共制作了10条调查性剖面图(RL),总长度为1.5 km,其中2条为贝拉沃达河纵向剖面图,8条为河流本身的横向或正剖面。沿着研究剖面进行现场扫描,采用地震波激励步骤,检波器距离为5 m,偏移量为10 m。地球物理调查结果证实,该区存在一小片上侏罗统花岗岩带,其中发育裂隙型含孔隙含水层。勘探(开发)钻孔建设的潜力区域有限,提出了四个潜在位置。
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Seismic explorations on the Bela Voda locality near Berovo
A b s t r a c t: This paper presents the results from the explorations conducted on the locality Bela Voda, village Dvorište near Berovo. The purpose of the site survey is to determine the potential of the water supplying with underground water according to the represented structural-tectonic and hydrogeological structure, locate and prognostically design exploratory wells for water supply according to the indicated potential, conditions and opportunities for ground water capture. For the needs of the geophysical measurements, field hydrogeological reconnaissance of the terrain has been performed previously. Hydrogeological research and geophysical measurements have been conducted on the locations where hydrogeological characteristics of the terrain and the presence of the types of water bearing environments within the research area have been defined and explained. The investigations are performed by means of reflective seismic scanning of the structural-tectonic assemblage on the terrain by representative investigative profiles and analysis of the known geological data. 10 investigative profiles (RL) with the total length of 1.5 km were made, of which 2 in the longitudinal direction of the Bela Voda river and 8 in the transverse or normal profiles of the river itself. The field scanning along the investigative profiles was performed with a seismic wave excitation step and a 5 m distance of geophones and an offset of 10 m. The obtained results from the performed geophysical investigations have confirmed that there is a small zone of Upper Jurassic granite in which a fissure type of aquifer with fissure porosity is formed. For the construction of well exploration (exploitation boreholes) there is a limited potential area, and four potential locations are proposed.
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来源期刊
Geologica Macedonica
Geologica Macedonica Earth and Planetary Sciences-Earth and Planetary Sciences (all)
CiteScore
0.60
自引率
0.00%
发文量
1
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