The Pannon LitH2Oscope magnetotelluric array in the Pannonian Basin
The Pannonian Basin is one of the best natural laboratories in the world to study the lithospheric response to continental extension and subsequent tectonic inversion. Here we address the topic of lithospheric structure by a combined geochemical and magnetotelluric analysis, which has been carried o...
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| Veröffentlicht in: | Acta geodaetica et geophysica 2024, Vol.59 (3), p.285-310 |
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| creator | Rubóczki, Tibor Novák, Attila Liptai, Nóra Porkoláb, Kristóf Molnár, Csaba Galsa, Attila Molnár, Gábor Wesztergom, Viktor Kovács, István János |
| description | The Pannonian Basin is one of the best natural laboratories in the world to study the lithospheric response to continental extension and subsequent tectonic inversion. Here we address the topic of lithospheric structure by a combined geochemical and magnetotelluric analysis, which has been carried out in the framework of the Pannon LitH
2
Oscope project. The main objective was to detect the resistivity distribution over the entire lithosphere by magnetotelluric measurements, considering the lithological resistivity properties and relate the results to the structure and evolution of the Pannonian Basin. The Pannon LitH
2
Oscope MT array was used to estimate the depth of the Lithosphere-Asthenosphere Boundary (LAB), considering the legacy MT data and compared to previous estimates for the region. Using the MT and geomagnetic response functions, major structural zones of the Pannonian basin, such as the Mid-Hungarian Shear Zone or fault systems like the Makó Trough and the Békés Basin, were also imaged. In addition, we used the apparent resistivity soundings to compare 1D resistivity models computed from geochemistry and obtained from field MT measurements. This comparison provided new constrains for the composition, fluid and melt content variations at the local lithosphere-asthenosphere boundary. The Pannon LitH
2
Oscope MT dataset and the results presented in this paper provide input for more complex 3D inversions and further investigations of the lithospheric structure in the Carpathian-Pannonian region. |
| doi_str_mv | 10.1007/s40328-024-00434-1 |
| format | Article |
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2
Oscope project. The main objective was to detect the resistivity distribution over the entire lithosphere by magnetotelluric measurements, considering the lithological resistivity properties and relate the results to the structure and evolution of the Pannonian Basin. The Pannon LitH
2
Oscope MT array was used to estimate the depth of the Lithosphere-Asthenosphere Boundary (LAB), considering the legacy MT data and compared to previous estimates for the region. Using the MT and geomagnetic response functions, major structural zones of the Pannonian basin, such as the Mid-Hungarian Shear Zone or fault systems like the Makó Trough and the Békés Basin, were also imaged. In addition, we used the apparent resistivity soundings to compare 1D resistivity models computed from geochemistry and obtained from field MT measurements. This comparison provided new constrains for the composition, fluid and melt content variations at the local lithosphere-asthenosphere boundary. The Pannon LitH
2
Oscope MT dataset and the results presented in this paper provide input for more complex 3D inversions and further investigations of the lithospheric structure in the Carpathian-Pannonian region.</description><identifier>ISSN: 2213-5812</identifier><identifier>EISSN: 2213-5820</identifier><identifier>DOI: 10.1007/s40328-024-00434-1</identifier><language>eng</language><publisher>Cham: Springer International Publishing</publisher><subject>Arrays ; Asthenosphere ; Earth and Environmental Science ; Earth Sciences ; Electrical resistivity ; Geochemistry ; Geophysics/Geodesy ; Inversions ; Lithology ; Lithosphere ; Magnetic properties ; Original Study ; Response functions ; Shear zone ; Soundings ; Tectonics</subject><ispartof>Acta geodaetica et geophysica, 2024, Vol.59 (3), p.285-310</ispartof><rights>The Author(s) 2024</rights><rights>The Author(s) 2024. This work is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c314t-47005701124c08897121700917f7933d19ced29ce34fa33b8db4125ad32ea5de3</cites><orcidid>0000-0002-2464-2468 ; 0000-0002-3488-3716 ; 0009-0008-1937-2580 ; 0000-0003-3489-3401 ; 0000-0001-7470-8296</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s40328-024-00434-1$$EPDF$$P50$$Gspringer$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s40328-024-00434-1$$EHTML$$P50$$Gspringer$$Hfree_for_read</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Rubóczki, Tibor</creatorcontrib><creatorcontrib>Novák, Attila</creatorcontrib><creatorcontrib>Liptai, Nóra</creatorcontrib><creatorcontrib>Porkoláb, Kristóf</creatorcontrib><creatorcontrib>Molnár, Csaba</creatorcontrib><creatorcontrib>Galsa, Attila</creatorcontrib><creatorcontrib>Molnár, Gábor</creatorcontrib><creatorcontrib>Wesztergom, Viktor</creatorcontrib><creatorcontrib>Kovács, István János</creatorcontrib><title>The Pannon LitH2Oscope magnetotelluric array in the Pannonian Basin</title><title>Acta geodaetica et geophysica</title><addtitle>Acta Geod Geophys</addtitle><description>The Pannonian Basin is one of the best natural laboratories in the world to study the lithospheric response to continental extension and subsequent tectonic inversion. Here we address the topic of lithospheric structure by a combined geochemical and magnetotelluric analysis, which has been carried out in the framework of the Pannon LitH
2
Oscope project. The main objective was to detect the resistivity distribution over the entire lithosphere by magnetotelluric measurements, considering the lithological resistivity properties and relate the results to the structure and evolution of the Pannonian Basin. The Pannon LitH
2
Oscope MT array was used to estimate the depth of the Lithosphere-Asthenosphere Boundary (LAB), considering the legacy MT data and compared to previous estimates for the region. Using the MT and geomagnetic response functions, major structural zones of the Pannonian basin, such as the Mid-Hungarian Shear Zone or fault systems like the Makó Trough and the Békés Basin, were also imaged. In addition, we used the apparent resistivity soundings to compare 1D resistivity models computed from geochemistry and obtained from field MT measurements. This comparison provided new constrains for the composition, fluid and melt content variations at the local lithosphere-asthenosphere boundary. The Pannon LitH
2
Oscope MT dataset and the results presented in this paper provide input for more complex 3D inversions and further investigations of the lithospheric structure in the Carpathian-Pannonian region.</description><subject>Arrays</subject><subject>Asthenosphere</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Electrical resistivity</subject><subject>Geochemistry</subject><subject>Geophysics/Geodesy</subject><subject>Inversions</subject><subject>Lithology</subject><subject>Lithosphere</subject><subject>Magnetic properties</subject><subject>Original Study</subject><subject>Response functions</subject><subject>Shear zone</subject><subject>Soundings</subject><subject>Tectonics</subject><issn>2213-5812</issn><issn>2213-5820</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><sourceid>C6C</sourceid><recordid>eNp9kMFKAzEQhoMoWGpfwFPAc3QmkyWboxa1QqEe6jmku9m6pc3WZHvo25u6Um9eJkP4_n_gY-wW4R4B9ENSQLIUIJUAUKQEXrCRlEiiKCVcnneU12yS0gYAsETURTFi0-Wn5-8uhC7wedvP5CJV3d7znVsH33e9324Psa24i9EdeRt4f-ZbF_iTS224YVeN2yY_-X3H7OPleTmdifni9W36OBcVoeqF0gCFBkSpKihLo1Fi_jKoG22IajSVr2UepBpHtCrrlUJZuJqkd0Xtaczuht597L4OPvV20x1iyCctgTG51yjMlByoKnYpRd_YfWx3Lh4tgj35soMvm33ZH1_2FKIhlDIc1j7-Vf-T-gaVP2r3</recordid><startdate>2024</startdate><enddate>2024</enddate><creator>Rubóczki, Tibor</creator><creator>Novák, Attila</creator><creator>Liptai, Nóra</creator><creator>Porkoláb, Kristóf</creator><creator>Molnár, Csaba</creator><creator>Galsa, Attila</creator><creator>Molnár, Gábor</creator><creator>Wesztergom, Viktor</creator><creator>Kovács, István János</creator><general>Springer International Publishing</general><general>Springer Nature B.V</general><scope>C6C</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><orcidid>https://orcid.org/0000-0002-2464-2468</orcidid><orcidid>https://orcid.org/0000-0002-3488-3716</orcidid><orcidid>https://orcid.org/0009-0008-1937-2580</orcidid><orcidid>https://orcid.org/0000-0003-3489-3401</orcidid><orcidid>https://orcid.org/0000-0001-7470-8296</orcidid></search><sort><creationdate>2024</creationdate><title>The Pannon LitH2Oscope magnetotelluric array in the Pannonian Basin</title><author>Rubóczki, Tibor ; Novák, Attila ; Liptai, Nóra ; Porkoláb, Kristóf ; Molnár, Csaba ; Galsa, Attila ; Molnár, Gábor ; Wesztergom, Viktor ; Kovács, István János</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c314t-47005701124c08897121700917f7933d19ced29ce34fa33b8db4125ad32ea5de3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>Arrays</topic><topic>Asthenosphere</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Electrical resistivity</topic><topic>Geochemistry</topic><topic>Geophysics/Geodesy</topic><topic>Inversions</topic><topic>Lithology</topic><topic>Lithosphere</topic><topic>Magnetic properties</topic><topic>Original Study</topic><topic>Response functions</topic><topic>Shear zone</topic><topic>Soundings</topic><topic>Tectonics</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Rubóczki, Tibor</creatorcontrib><creatorcontrib>Novák, Attila</creatorcontrib><creatorcontrib>Liptai, Nóra</creatorcontrib><creatorcontrib>Porkoláb, Kristóf</creatorcontrib><creatorcontrib>Molnár, Csaba</creatorcontrib><creatorcontrib>Galsa, Attila</creatorcontrib><creatorcontrib>Molnár, Gábor</creatorcontrib><creatorcontrib>Wesztergom, Viktor</creatorcontrib><creatorcontrib>Kovács, István János</creatorcontrib><collection>Springer Nature OA Free Journals</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Acta geodaetica et geophysica</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Rubóczki, Tibor</au><au>Novák, Attila</au><au>Liptai, Nóra</au><au>Porkoláb, Kristóf</au><au>Molnár, Csaba</au><au>Galsa, Attila</au><au>Molnár, Gábor</au><au>Wesztergom, Viktor</au><au>Kovács, István János</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The Pannon LitH2Oscope magnetotelluric array in the Pannonian Basin</atitle><jtitle>Acta geodaetica et geophysica</jtitle><stitle>Acta Geod Geophys</stitle><date>2024</date><risdate>2024</risdate><volume>59</volume><issue>3</issue><spage>285</spage><epage>310</epage><pages>285-310</pages><issn>2213-5812</issn><eissn>2213-5820</eissn><abstract>The Pannonian Basin is one of the best natural laboratories in the world to study the lithospheric response to continental extension and subsequent tectonic inversion. Here we address the topic of lithospheric structure by a combined geochemical and magnetotelluric analysis, which has been carried out in the framework of the Pannon LitH
2
Oscope project. The main objective was to detect the resistivity distribution over the entire lithosphere by magnetotelluric measurements, considering the lithological resistivity properties and relate the results to the structure and evolution of the Pannonian Basin. The Pannon LitH
2
Oscope MT array was used to estimate the depth of the Lithosphere-Asthenosphere Boundary (LAB), considering the legacy MT data and compared to previous estimates for the region. Using the MT and geomagnetic response functions, major structural zones of the Pannonian basin, such as the Mid-Hungarian Shear Zone or fault systems like the Makó Trough and the Békés Basin, were also imaged. In addition, we used the apparent resistivity soundings to compare 1D resistivity models computed from geochemistry and obtained from field MT measurements. This comparison provided new constrains for the composition, fluid and melt content variations at the local lithosphere-asthenosphere boundary. The Pannon LitH
2
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| subjects | Arrays Asthenosphere Earth and Environmental Science Earth Sciences Electrical resistivity Geochemistry Geophysics/Geodesy Inversions Lithology Lithosphere Magnetic properties Original Study Response functions Shear zone Soundings Tectonics |
| title | The Pannon LitH2Oscope magnetotelluric array in the Pannonian Basin |
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