High‐resolution stratigraphy of Quaternary fluvial deposits in the Makó Trough and the Danube‐Tisza Interfluve, Hungary, based on magnetic susceptibility data
High‐resolution stratigraphical architecture of a Quaternary fluvial succession in the Makó Trough and the Danube‐Tisza Interfluve (Pannonian Basin, Hungary) was investigated based on low field magnetic susceptibility ( MS ) measurements of seven fully cored boreholes, interpreted on the basis of th...
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crwiley:10.1111/bor.12471 2024-06-02T08:13:08+00:00 High‐resolution stratigraphy of Quaternary fluvial deposits in the Makó Trough and the Danube‐Tisza Interfluve, Hungary, based on magnetic susceptibility data Püspöki, Zoltán Fogarassy‐Pummer, Tímea Thamó‐Bozsó, Edit Falus, György Cserkész‐Nagy, Ágnes Szappanos, Bálint Márton, Emő Lantos, Zoltán Szabó, Szilárd Stercel, Ferenc Tóth‐Makk, Ágnes Mcintosh, Richard W. Szőcs, Teodóra Pálóczy, Péter Fancsik, Tamás 2020 http://dx.doi.org/10.1111/bor.12471 https://onlinelibrary.wiley.com/doi/pdf/10.1111/bor.12471 https://onlinelibrary.wiley.com/doi/full-xml/10.1111/bor.12471 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Boreas volume 50, issue 1, page 205-223 ISSN 0300-9483 1502-3885 journal-article 2020 crwiley https://doi.org/10.1111/bor.12471 2024-05-03T12:03:22Z High‐resolution stratigraphical architecture of a Quaternary fluvial succession in the Makó Trough and the Danube‐Tisza Interfluve (Pannonian Basin, Hungary) was investigated based on low field magnetic susceptibility ( MS ) measurements of seven fully cored boreholes, interpreted on the basis of the early postglacial magnetic susceptibility episodes previously described in the Körös and Jászság Basins. To confirm the reliability of the Dévaványa and Vésztő MS records (Körös Basin), the published magnetostratigraphical data were re‐investigated revealing the consequent arrangement of the MS peaks correlated with the Jingbian section and the short‐lived polarity reversals correlated with the Geomagnetic Instability Time Scale. The Quaternary climatic regime in the Körös Basin begins in the late Pliocene at 2.7 Ma. The correlation between the Körös Basin (Dévaványa) and Makó Trough (Mindszent) was confirmed by the multi‐proxy spectral investigation of the Mindszent section, revealing ~100‐ and ~41‐ka cycles in the MS , colour, logged spontaneous potential and resistivity records. Based on MS records of the seven boreholes, the base of the Quaternary can be identified irrespective of the facies, age and climatic phase of the lowermost Quaternary strata. By performing MS and log correlation of 131 boreholes, extended unconformities were detected in the Quaternary profiles in the Danube‐Tisza Interfluve (~1070±10, ~1920±10 and ~2300±10 ka) interpreted as sequence boundaries. Sedimentological and mineralogical data reveal a significant change at ~725–606 ka likely as a response to the ‘mid‐Pleistocene transition’, leading to the multiple branching of the Danube. SEM data revealed that ilmenite is also responsible for the development of the early postglacial magnetic susceptibility episodes. This increases the stratigraphical potential of fluvial successions with catchment area that contain metamorphic rocks. A gradual retreat of permafrost zone determines long‐term temporal trends of the climatically controlled ... Article in Journal/Newspaper permafrost Wiley Online Library Boreas 50 1 205 223 |
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English |
description |
High‐resolution stratigraphical architecture of a Quaternary fluvial succession in the Makó Trough and the Danube‐Tisza Interfluve (Pannonian Basin, Hungary) was investigated based on low field magnetic susceptibility ( MS ) measurements of seven fully cored boreholes, interpreted on the basis of the early postglacial magnetic susceptibility episodes previously described in the Körös and Jászság Basins. To confirm the reliability of the Dévaványa and Vésztő MS records (Körös Basin), the published magnetostratigraphical data were re‐investigated revealing the consequent arrangement of the MS peaks correlated with the Jingbian section and the short‐lived polarity reversals correlated with the Geomagnetic Instability Time Scale. The Quaternary climatic regime in the Körös Basin begins in the late Pliocene at 2.7 Ma. The correlation between the Körös Basin (Dévaványa) and Makó Trough (Mindszent) was confirmed by the multi‐proxy spectral investigation of the Mindszent section, revealing ~100‐ and ~41‐ka cycles in the MS , colour, logged spontaneous potential and resistivity records. Based on MS records of the seven boreholes, the base of the Quaternary can be identified irrespective of the facies, age and climatic phase of the lowermost Quaternary strata. By performing MS and log correlation of 131 boreholes, extended unconformities were detected in the Quaternary profiles in the Danube‐Tisza Interfluve (~1070±10, ~1920±10 and ~2300±10 ka) interpreted as sequence boundaries. Sedimentological and mineralogical data reveal a significant change at ~725–606 ka likely as a response to the ‘mid‐Pleistocene transition’, leading to the multiple branching of the Danube. SEM data revealed that ilmenite is also responsible for the development of the early postglacial magnetic susceptibility episodes. This increases the stratigraphical potential of fluvial successions with catchment area that contain metamorphic rocks. A gradual retreat of permafrost zone determines long‐term temporal trends of the climatically controlled ... |
format |
Article in Journal/Newspaper |
author |
Püspöki, Zoltán Fogarassy‐Pummer, Tímea Thamó‐Bozsó, Edit Falus, György Cserkész‐Nagy, Ágnes Szappanos, Bálint Márton, Emő Lantos, Zoltán Szabó, Szilárd Stercel, Ferenc Tóth‐Makk, Ágnes Mcintosh, Richard W. Szőcs, Teodóra Pálóczy, Péter Fancsik, Tamás |
spellingShingle |
Püspöki, Zoltán Fogarassy‐Pummer, Tímea Thamó‐Bozsó, Edit Falus, György Cserkész‐Nagy, Ágnes Szappanos, Bálint Márton, Emő Lantos, Zoltán Szabó, Szilárd Stercel, Ferenc Tóth‐Makk, Ágnes Mcintosh, Richard W. Szőcs, Teodóra Pálóczy, Péter Fancsik, Tamás High‐resolution stratigraphy of Quaternary fluvial deposits in the Makó Trough and the Danube‐Tisza Interfluve, Hungary, based on magnetic susceptibility data |
author_facet |
Püspöki, Zoltán Fogarassy‐Pummer, Tímea Thamó‐Bozsó, Edit Falus, György Cserkész‐Nagy, Ágnes Szappanos, Bálint Márton, Emő Lantos, Zoltán Szabó, Szilárd Stercel, Ferenc Tóth‐Makk, Ágnes Mcintosh, Richard W. Szőcs, Teodóra Pálóczy, Péter Fancsik, Tamás |
author_sort |
Püspöki, Zoltán |
title |
High‐resolution stratigraphy of Quaternary fluvial deposits in the Makó Trough and the Danube‐Tisza Interfluve, Hungary, based on magnetic susceptibility data |
title_short |
High‐resolution stratigraphy of Quaternary fluvial deposits in the Makó Trough and the Danube‐Tisza Interfluve, Hungary, based on magnetic susceptibility data |
title_full |
High‐resolution stratigraphy of Quaternary fluvial deposits in the Makó Trough and the Danube‐Tisza Interfluve, Hungary, based on magnetic susceptibility data |
title_fullStr |
High‐resolution stratigraphy of Quaternary fluvial deposits in the Makó Trough and the Danube‐Tisza Interfluve, Hungary, based on magnetic susceptibility data |
title_full_unstemmed |
High‐resolution stratigraphy of Quaternary fluvial deposits in the Makó Trough and the Danube‐Tisza Interfluve, Hungary, based on magnetic susceptibility data |
title_sort |
high‐resolution stratigraphy of quaternary fluvial deposits in the makó trough and the danube‐tisza interfluve, hungary, based on magnetic susceptibility data |
publisher |
Wiley |
publishDate |
2020 |
url |
http://dx.doi.org/10.1111/bor.12471 https://onlinelibrary.wiley.com/doi/pdf/10.1111/bor.12471 https://onlinelibrary.wiley.com/doi/full-xml/10.1111/bor.12471 |
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permafrost |
genre_facet |
permafrost |
op_source |
Boreas volume 50, issue 1, page 205-223 ISSN 0300-9483 1502-3885 |
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http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/bor.12471 |
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