Applications of shallow seismic refraction measurements in the Western Carpathians (Slovakia): case studies

Shallow seismic measurement, specifically seismic refraction tomography, is an effective geophysical method that has applications in various sectors. It enables the search for and determination of the course of the interfaces, thus helping to resolve geological, environmental, hydrogeological, engin...
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Autor*in:	Bibiana BRIXOVÁ [verfasserIn] Andrea MOSNÁ [verfasserIn] René PUTIŠKA [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2018

Schlagwörter:	refraction seismics, seismic refraction tomography, shallow seismic measurements, western carpathians, case study

Übergeordnetes Werk:	In: Contributions to Geophysics and Geodesy - Earth Science Institute, Slovak Academy of Sciences, Slovakia, 2020, 48(2018), 1, Seite 21
Übergeordnetes Werk:	volume:48 ; year:2018 ; number:1 ; pages:21

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.2478/congeo-2018-0001

Katalog-ID:	DOAJ034390677

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spellingShingle	Bibiana BRIXOVÁ misc QB275-343 misc QC801-809 misc refraction seismics, seismic refraction tomography, shallow seismic measurements, western carpathians, case study misc Geodesy misc Geophysics. Cosmic physics Applications of shallow seismic refraction measurements in the Western Carpathians (Slovakia): case studies
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topic_title	QB275-343 QC801-809 Applications of shallow seismic refraction measurements in the Western Carpathians (Slovakia): case studies refraction seismics, seismic refraction tomography, shallow seismic measurements, western carpathians, case study
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title	Applications of shallow seismic refraction measurements in the Western Carpathians (Slovakia): case studies
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title_sort	applications of shallow seismic refraction measurements in the western carpathians (slovakia): case studies
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title_auth	Applications of shallow seismic refraction measurements in the Western Carpathians (Slovakia): case studies
abstract	Shallow seismic measurement, specifically seismic refraction tomography, is an effective geophysical method that has applications in various sectors. It enables the search for and determination of the course of the interfaces, thus helping to resolve geological, environmental, hydrogeological, engineering, geotechnical and other problems. The paper demonstrates the possibilities of using these methods through examples of shallow seismic measurements that have been performed at various four locations in the Western Carpathian Mountains. The first case study describes Monastery Pond at Katarínka. It was found that, the basement of the Monastery pond is at a depth of 2–3 m below the surface and the results were also confirmed by electrical resistivity tomography (ERT). The next measurement through the thermal power station waste storage showed that the storage area base runs at a depth of about 20 m under the measured profile. The third case study addresses the depth of groundwater depth in the area of Borská nížina. The measurement confirmed the assumed depth of ground water level at 3.35 m below the surface. In the last case study, border fault between the Turiec Basin and the Malá Fatra Mts. was mapped by application of shallow refraction methods. The results show that shallow seismic methods shed light on the problem and in combination with other geophysical methods are an effective tool with great potential. They provide very useful data for shallow mapping applications.
abstractGer	Shallow seismic measurement, specifically seismic refraction tomography, is an effective geophysical method that has applications in various sectors. It enables the search for and determination of the course of the interfaces, thus helping to resolve geological, environmental, hydrogeological, engineering, geotechnical and other problems. The paper demonstrates the possibilities of using these methods through examples of shallow seismic measurements that have been performed at various four locations in the Western Carpathian Mountains. The first case study describes Monastery Pond at Katarínka. It was found that, the basement of the Monastery pond is at a depth of 2–3 m below the surface and the results were also confirmed by electrical resistivity tomography (ERT). The next measurement through the thermal power station waste storage showed that the storage area base runs at a depth of about 20 m under the measured profile. The third case study addresses the depth of groundwater depth in the area of Borská nížina. The measurement confirmed the assumed depth of ground water level at 3.35 m below the surface. In the last case study, border fault between the Turiec Basin and the Malá Fatra Mts. was mapped by application of shallow refraction methods. The results show that shallow seismic methods shed light on the problem and in combination with other geophysical methods are an effective tool with great potential. They provide very useful data for shallow mapping applications.
abstract_unstemmed	Shallow seismic measurement, specifically seismic refraction tomography, is an effective geophysical method that has applications in various sectors. It enables the search for and determination of the course of the interfaces, thus helping to resolve geological, environmental, hydrogeological, engineering, geotechnical and other problems. The paper demonstrates the possibilities of using these methods through examples of shallow seismic measurements that have been performed at various four locations in the Western Carpathian Mountains. The first case study describes Monastery Pond at Katarínka. It was found that, the basement of the Monastery pond is at a depth of 2–3 m below the surface and the results were also confirmed by electrical resistivity tomography (ERT). The next measurement through the thermal power station waste storage showed that the storage area base runs at a depth of about 20 m under the measured profile. The third case study addresses the depth of groundwater depth in the area of Borská nížina. The measurement confirmed the assumed depth of ground water level at 3.35 m below the surface. In the last case study, border fault between the Turiec Basin and the Malá Fatra Mts. was mapped by application of shallow refraction methods. The results show that shallow seismic methods shed light on the problem and in combination with other geophysical methods are an effective tool with great potential. They provide very useful data for shallow mapping applications.
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title_short	Applications of shallow seismic refraction measurements in the Western Carpathians (Slovakia): case studies
url	https://doi.org/10.2478/congeo-2018-0001 https://doaj.org/article/6caad92ae3cd47fe9023f1faeedf7517 https://journal.geo.sav.sk/cgg/article/view/176 https://doaj.org/toc/1338-0540
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Applications of shallow seismic refraction measurements in the Western Carpathians (Slovakia): case studies

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