DC pole | Wartość | Język |
dc.contributor.author | Mendecki, Maciej J. | - |
dc.contributor.author | Zuberek, Wacław M. | - |
dc.contributor.author | Hrehorowicz, Przemysław | - |
dc.contributor.author | Jarek, Szymon | - |
dc.date.accessioned | 2020-04-22T06:30:13Z | - |
dc.date.available | 2020-04-22T06:30:13Z | - |
dc.date.issued | 2012 | - |
dc.identifier.citation | Contemporary Trends in Geoscience, Vol. 1 (2012), s. 39-44 | pl_PL |
dc.identifier.issn | 2084-5707 | - |
dc.identifier.issn | 2299-8179 | - |
dc.identifier.uri | http://hdl.handle.net/20.500.12128/13588 | - |
dc.description.abstract | Identification of a bedrock beneath soft cover is one of the most important task in engineering geology. The
location of boundary-overburden information may be used by investors, builders and municipal authorities to design an infrastructure or land-use plans. In such issues the application of appropriate geophysical methods is useful. However, in urban zones and areas characterized by subsurface soft layer the usage of certain methods (eg.: seismic refraction) is not advisable. The passive method of Refraction Microtremor (ReMi) can fulfill its tasks in the relatively difficult urban environment. The vertical S-wave velocity profiles were carried out as a result of inversion of Rayleigh wave dispersion curves obtained from ReMi method. The change of S-wave velocities allowed to distinguish shallow geological layers in the area of Chorzów Stary. Preliminary measurements allowed to identify the Carboniferous bedrock at a depth of 14 -18 m what
has been confirmed by resistivity imaging. Furthermore, unconsolidated deposits are also recognized and the seismic results show a good correlation with the available geological information and resistivity imaging data. | pl_PL |
dc.language.iso | en | pl_PL |
dc.rights | Uznanie autorstwa-Użycie niekomercyjne-Bez utworów zależnych 3.0 Polska | * |
dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/3.0/pl/ | * |
dc.subject | Ambient seismic noise | pl_PL |
dc.subject | ReMi | pl_PL |
dc.subject | resistivity imaging | pl_PL |
dc.subject | bedrock-overburden boundary | pl_PL |
dc.subject | Chorzów Stary | pl_PL |
dc.title | An inversion of rayleigh waves dispersion curves as a tool to recognize the bedrock depth in Chorzów Stary, Poland | pl_PL |
dc.type | info:eu-repo/semantics/article | pl_PL |
dc.identifier.doi | 10.2478/ctg-2012-0005 | - |
Pojawia się w kolekcji: | Artykuły (WNP)
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