TY - JOUR AU - Tan, Xin AU - Meng, Qingyan AU - Zhao, Fei AU - Zhang, Linlin AU - Hu, Xinli AU - Jancsó, Tamás TI - HR-UVFormer: A top-down and multimodal hierarchical extraction approach for urban villages JF - IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING J2 - IEEE T GEOSCI REMOTE PY - 2024 PG - 15 SN - 0196-2892 DO - 10.1109/TGRS.2024.3387022 UR - https://m2.mtmt.hu/api/publication/34814642 ID - 34814642 LA - English DB - MTMT ER - TY - JOUR AU - Rubóczki, Tibor AU - Novák, Attila AU - Liptai, Nóra AU - Porkoláb, Kristóf AU - Molnár, Csaba AU - Galsa, Attila AU - Molnár, Gábor AU - Wesztergom, Viktor AU - Kovács, István János TI - The Pannon LitH2Oscope magnetotelluric array in the Pannonian Basin JF - ACTA GEODAETICA ET GEOPHYSICA J2 - ACTA GEOD GEOPHYS PY - 2024 PG - 26 SN - 2213-5812 DO - 10.1007/s40328-024-00434-1 UR - https://m2.mtmt.hu/api/publication/34608098 ID - 34608098 N1 - HUN-REN Institute of Earth Physics and Space Science, Sopron, Hungary MTA FI Lendület Pannon LitH2Oscope Research Group, Sopron, Hungary Doctoral School of Earth Sciences, Eötvös Loránd University, Budapest, Hungary Department of Geophysics and Space Science, Institute of Geography and Earth Sciences, ELTE Eötvös Loránd University, Budapest, Hungary Alba Regia Technical Faculty, Institute of Geoinformatics, Óbuda University, Székesfehérvár, Hungary Export Date: 25 March 2024 Correspondence Address: Rubóczki, T.; HUN-REN Institute of Earth Physics and Space ScienceHungary; email: ruboczki.tibor@epss.hun-ren.hu AB - 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 LitH2Oscope 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. 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