Eintrag weiter verarbeiten
Geological interpretation of magnetotelluric sounding in the southern part of seismic profile 2T (Central Slovakia)
Gespeichert in:
| Zeitschriftentitel: | Contributions to Geophysics and Geodesy |
|---|---|
| Personen und Körperschaften: | , , , , , , |
| In: | Contributions to Geophysics and Geodesy, 45, 2015, 1, S. 1-11 |
| Format: | E-Article |
| Sprache: | Unbestimmt |
| veröffentlicht: |
Central Library of the Slovak Academy of Sciences
|
| Schlagwörter: |
| author_facet |
Bezák, Vladimír Pek, Josef Majcin, Dušan Bučová, Jana Šoltis, Tomáš Bilčík, Dušan Klanica, Radek Bezák, Vladimír Pek, Josef Majcin, Dušan Bučová, Jana Šoltis, Tomáš Bilčík, Dušan Klanica, Radek |
|---|---|
| author |
Bezák, Vladimír Pek, Josef Majcin, Dušan Bučová, Jana Šoltis, Tomáš Bilčík, Dušan Klanica, Radek |
| spellingShingle |
Bezák, Vladimír Pek, Josef Majcin, Dušan Bučová, Jana Šoltis, Tomáš Bilčík, Dušan Klanica, Radek Contributions to Geophysics and Geodesy Geological interpretation of magnetotelluric sounding in the southern part of seismic profile 2T (Central Slovakia) Geophysics |
| author_sort |
bezák, vladimír |
| spelling |
Bezák, Vladimír Pek, Josef Majcin, Dušan Bučová, Jana Šoltis, Tomáš Bilčík, Dušan Klanica, Radek 1338-0540 Central Library of the Slovak Academy of Sciences Geophysics http://dx.doi.org/10.1515/congeo-2015-0009 <jats:title>Abstract</jats:title> <jats:p> In this paper we present a geological interpretation of magnetotelluric sounding along the southern part of the seismic 2T profile situated in the southern Central Slovakia. The complexes with higher conductivity are imaged in the shallow depths, formed by the Tertiary sediments and volcanics. In the northernmost part of the profile, the influence of non-conductive complexes composed of orthogneisses and overlying Mesozoic carbonates is significant. In the central part of the profile, the low conductive granitoid complexes are superposed over the metamorphic rocks with higher conductivity. This structure is a remnant of the Hercynian middle crust nappes. The most outstanding phenomenon of the profile is the sudden, almost step change in the conductivity parameters of the crust in the southern part. The significantly high conductivity of the crust in this area is most probably not related to its lithological composition, but by the abundant supply of fluids in the crust connected with the Neogene tectonic and volcanic processes.</jats:p> Geological interpretation of magnetotelluric sounding in the southern part of seismic profile 2T (Central Slovakia) Contributions to Geophysics and Geodesy |
| doi_str_mv |
10.1515/congeo-2015-0009 |
| facet_avail |
Online Free |
| finc_class_facet |
Physik Geologie und Paläontologie Geographie |
| format |
ElectronicArticle |
| fullrecord |
blob:ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTUxNS9jb25nZW8tMjAxNS0wMDA5 |
| id |
ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTUxNS9jb25nZW8tMjAxNS0wMDA5 |
| institution |
DE-Gla1 DE-Zi4 DE-15 DE-Pl11 DE-Rs1 DE-105 DE-14 DE-Ch1 DE-L229 DE-D275 DE-Bn3 DE-Brt1 DE-Zwi2 DE-D161 |
| imprint |
Central Library of the Slovak Academy of Sciences, 2015 |
| imprint_str_mv |
Central Library of the Slovak Academy of Sciences, 2015 |
| issn |
1338-0540 |
| issn_str_mv |
1338-0540 |
| language |
Undetermined |
| mega_collection |
Central Library of the Slovak Academy of Sciences (CrossRef) |
| match_str |
bezak2015geologicalinterpretationofmagnetotelluricsoundinginthesouthernpartofseismicprofile2tcentralslovakia |
| publishDateSort |
2015 |
| publisher |
Central Library of the Slovak Academy of Sciences |
| recordtype |
ai |
| record_format |
ai |
| series |
Contributions to Geophysics and Geodesy |
| source_id |
49 |
| title |
Geological interpretation of magnetotelluric sounding in the southern part of seismic profile 2T (Central Slovakia) |
| title_unstemmed |
Geological interpretation of magnetotelluric sounding in the southern part of seismic profile 2T (Central Slovakia) |
| title_full |
Geological interpretation of magnetotelluric sounding in the southern part of seismic profile 2T (Central Slovakia) |
| title_fullStr |
Geological interpretation of magnetotelluric sounding in the southern part of seismic profile 2T (Central Slovakia) |
| title_full_unstemmed |
Geological interpretation of magnetotelluric sounding in the southern part of seismic profile 2T (Central Slovakia) |
| title_short |
Geological interpretation of magnetotelluric sounding in the southern part of seismic profile 2T (Central Slovakia) |
| title_sort |
geological interpretation of magnetotelluric sounding in the southern part of seismic profile 2t (central slovakia) |
| topic |
Geophysics |
| url |
http://dx.doi.org/10.1515/congeo-2015-0009 |
| publishDate |
2015 |
| physical |
1-11 |
| description |
<jats:title>Abstract</jats:title>
<jats:p> In this paper we present a geological interpretation of magnetotelluric sounding along the southern part of the seismic 2T profile situated in the southern Central Slovakia. The complexes with higher conductivity are imaged in the shallow depths, formed by the Tertiary sediments and volcanics. In the northernmost part of the profile, the influence of non-conductive complexes composed of orthogneisses and overlying Mesozoic carbonates is significant. In the central part of the profile, the low conductive granitoid complexes are superposed over the metamorphic rocks with higher conductivity. This structure is a remnant of the Hercynian middle crust nappes. The most outstanding phenomenon of the profile is the sudden, almost step change in the conductivity parameters of the crust in the southern part. The significantly high conductivity of the crust in this area is most probably not related to its lithological composition, but by the abundant supply of fluids in the crust connected with the Neogene tectonic and volcanic processes.</jats:p> |
| container_issue |
1 |
| container_start_page |
1 |
| container_title |
Contributions to Geophysics and Geodesy |
| container_volume |
45 |
| format_de105 |
Article, E-Article |
| format_de14 |
Article, E-Article |
| format_de15 |
Article, E-Article |
| format_de520 |
Article, E-Article |
| format_de540 |
Article, E-Article |
| format_dech1 |
Article, E-Article |
| format_ded117 |
Article, E-Article |
| format_degla1 |
E-Article |
| format_del152 |
Buch |
| format_del189 |
Article, E-Article |
| format_dezi4 |
Article |
| format_dezwi2 |
Article, E-Article |
| format_finc |
Article, E-Article |
| format_nrw |
Article, E-Article |
| _version_ |
1792343624801845254 |
| geogr_code |
not assigned |
| last_indexed |
2024-03-01T16:54:39.222Z |
| geogr_code_person |
not assigned |
| openURL |
url_ver=Z39.88-2004&ctx_ver=Z39.88-2004&ctx_enc=info%3Aofi%2Fenc%3AUTF-8&rfr_id=info%3Asid%2Fvufind.svn.sourceforge.net%3Agenerator&rft.title=Geological+interpretation+of+magnetotelluric+sounding+in+the+southern+part+of+seismic+profile+2T+%28Central+Slovakia%29&rft.date=2015-03-01&genre=article&issn=1338-0540&volume=45&issue=1&spage=1&epage=11&pages=1-11&jtitle=Contributions+to+Geophysics+and+Geodesy&atitle=Geological+interpretation+of+magnetotelluric+sounding+in+the+southern+part+of+seismic+profile+2T+%28Central+Slovakia%29&aulast=Klanica&aufirst=Radek&rft_id=info%3Adoi%2F10.1515%2Fcongeo-2015-0009&rft.language%5B0%5D=und |
| SOLR | |
| _version_ | 1792343624801845254 |
| author | Bezák, Vladimír, Pek, Josef, Majcin, Dušan, Bučová, Jana, Šoltis, Tomáš, Bilčík, Dušan, Klanica, Radek |
| author_facet | Bezák, Vladimír, Pek, Josef, Majcin, Dušan, Bučová, Jana, Šoltis, Tomáš, Bilčík, Dušan, Klanica, Radek, Bezák, Vladimír, Pek, Josef, Majcin, Dušan, Bučová, Jana, Šoltis, Tomáš, Bilčík, Dušan, Klanica, Radek |
| author_sort | bezák, vladimír |
| container_issue | 1 |
| container_start_page | 1 |
| container_title | Contributions to Geophysics and Geodesy |
| container_volume | 45 |
| description | <jats:title>Abstract</jats:title> <jats:p> In this paper we present a geological interpretation of magnetotelluric sounding along the southern part of the seismic 2T profile situated in the southern Central Slovakia. The complexes with higher conductivity are imaged in the shallow depths, formed by the Tertiary sediments and volcanics. In the northernmost part of the profile, the influence of non-conductive complexes composed of orthogneisses and overlying Mesozoic carbonates is significant. In the central part of the profile, the low conductive granitoid complexes are superposed over the metamorphic rocks with higher conductivity. This structure is a remnant of the Hercynian middle crust nappes. The most outstanding phenomenon of the profile is the sudden, almost step change in the conductivity parameters of the crust in the southern part. The significantly high conductivity of the crust in this area is most probably not related to its lithological composition, but by the abundant supply of fluids in the crust connected with the Neogene tectonic and volcanic processes.</jats:p> |
| doi_str_mv | 10.1515/congeo-2015-0009 |
| facet_avail | Online, Free |
| finc_class_facet | Physik, Geologie und Paläontologie, Geographie |
| format | ElectronicArticle |
| format_de105 | Article, E-Article |
| format_de14 | Article, E-Article |
| format_de15 | Article, E-Article |
| format_de520 | Article, E-Article |
| format_de540 | Article, E-Article |
| format_dech1 | Article, E-Article |
| format_ded117 | Article, E-Article |
| format_degla1 | E-Article |
| format_del152 | Buch |
| format_del189 | Article, E-Article |
| format_dezi4 | Article |
| format_dezwi2 | Article, E-Article |
| format_finc | Article, E-Article |
| format_nrw | Article, E-Article |
| geogr_code | not assigned |
| geogr_code_person | not assigned |
| id | ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTUxNS9jb25nZW8tMjAxNS0wMDA5 |
| imprint | Central Library of the Slovak Academy of Sciences, 2015 |
| imprint_str_mv | Central Library of the Slovak Academy of Sciences, 2015 |
| institution | DE-Gla1, DE-Zi4, DE-15, DE-Pl11, DE-Rs1, DE-105, DE-14, DE-Ch1, DE-L229, DE-D275, DE-Bn3, DE-Brt1, DE-Zwi2, DE-D161 |
| issn | 1338-0540 |
| issn_str_mv | 1338-0540 |
| language | Undetermined |
| last_indexed | 2024-03-01T16:54:39.222Z |
| match_str | bezak2015geologicalinterpretationofmagnetotelluricsoundinginthesouthernpartofseismicprofile2tcentralslovakia |
| mega_collection | Central Library of the Slovak Academy of Sciences (CrossRef) |
| physical | 1-11 |
| publishDate | 2015 |
| publishDateSort | 2015 |
| publisher | Central Library of the Slovak Academy of Sciences |
| record_format | ai |
| recordtype | ai |
| series | Contributions to Geophysics and Geodesy |
| source_id | 49 |
| spelling | Bezák, Vladimír Pek, Josef Majcin, Dušan Bučová, Jana Šoltis, Tomáš Bilčík, Dušan Klanica, Radek 1338-0540 Central Library of the Slovak Academy of Sciences Geophysics http://dx.doi.org/10.1515/congeo-2015-0009 <jats:title>Abstract</jats:title> <jats:p> In this paper we present a geological interpretation of magnetotelluric sounding along the southern part of the seismic 2T profile situated in the southern Central Slovakia. The complexes with higher conductivity are imaged in the shallow depths, formed by the Tertiary sediments and volcanics. In the northernmost part of the profile, the influence of non-conductive complexes composed of orthogneisses and overlying Mesozoic carbonates is significant. In the central part of the profile, the low conductive granitoid complexes are superposed over the metamorphic rocks with higher conductivity. This structure is a remnant of the Hercynian middle crust nappes. The most outstanding phenomenon of the profile is the sudden, almost step change in the conductivity parameters of the crust in the southern part. The significantly high conductivity of the crust in this area is most probably not related to its lithological composition, but by the abundant supply of fluids in the crust connected with the Neogene tectonic and volcanic processes.</jats:p> Geological interpretation of magnetotelluric sounding in the southern part of seismic profile 2T (Central Slovakia) Contributions to Geophysics and Geodesy |
| spellingShingle | Bezák, Vladimír, Pek, Josef, Majcin, Dušan, Bučová, Jana, Šoltis, Tomáš, Bilčík, Dušan, Klanica, Radek, Contributions to Geophysics and Geodesy, Geological interpretation of magnetotelluric sounding in the southern part of seismic profile 2T (Central Slovakia), Geophysics |
| title | Geological interpretation of magnetotelluric sounding in the southern part of seismic profile 2T (Central Slovakia) |
| title_full | Geological interpretation of magnetotelluric sounding in the southern part of seismic profile 2T (Central Slovakia) |
| title_fullStr | Geological interpretation of magnetotelluric sounding in the southern part of seismic profile 2T (Central Slovakia) |
| title_full_unstemmed | Geological interpretation of magnetotelluric sounding in the southern part of seismic profile 2T (Central Slovakia) |
| title_short | Geological interpretation of magnetotelluric sounding in the southern part of seismic profile 2T (Central Slovakia) |
| title_sort | geological interpretation of magnetotelluric sounding in the southern part of seismic profile 2t (central slovakia) |
| title_unstemmed | Geological interpretation of magnetotelluric sounding in the southern part of seismic profile 2T (Central Slovakia) |
| topic | Geophysics |
| url | http://dx.doi.org/10.1515/congeo-2015-0009 |