@CONFERENCE{MTMT:34733990,
	title = {Hydrous nano-silicate melt inclusions supports amphibole growth, Persani Mountains Volcanic Field (Transylvania)},
	url = {https://m2.mtmt.hu/api/publication/34733990},
	author = {Lange, Thomas Pieter and Pálos, Zsófia and Berkesi, Márta and Pekker, Péter and Szabó, Ábel and Szabó, Csaba and Kovács, István János},
	booktitle = {EGU General Assembly 2024 : abstracts},
	unique-id = {34733990},
	year = {2024},
	pages = {EGU24-19855},
	orcid-numbers = {Lange, Thomas Pieter/0000-0002-8709-9239; Berkesi, Márta/0000-0003-4380-057X; Pekker, Péter/0000-0002-0463-0742; Szabó, Csaba/0000-0002-1580-6344; Kovács, István János/0000-0002-3488-3716}
}

@article{MTMT:34608098,
	title = {The Pannon LitH2Oscope magnetotelluric array in the Pannonian Basin},
	url = {https://m2.mtmt.hu/api/publication/34608098},
	author = {Rubóczki, Tibor and Novák, Attila and Liptai, Nóra and Porkoláb, Kristóf and Molnár, Csaba and Galsa, Attila and Molnár, Gábor and Wesztergom, Viktor and Kovács, István János},
	doi = {10.1007/s40328-024-00434-1},
	journal-iso = {ACTA GEOD GEOPHYS},
	journal = {ACTA GEODAETICA ET GEOPHYSICA},
	unique-id = {34608098},
	issn = {2213-5812},
	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 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.},
	year = {2024},
	eissn = {2213-5820},
	orcid-numbers = {Rubóczki, Tibor/0009-0008-1937-2580; Liptai, Nóra/0000-0002-2464-2468; Porkoláb, Kristóf/0000-0001-7470-8296; Galsa, Attila/0000-0002-7198-4524; Molnár, Gábor/0000-0001-9309-3418; Kovács, István János/0000-0002-3488-3716}
}

@article{MTMT:33785006,
	title = {Formation of amphibole lamellae in mantle pyroxene by fluid-mediated metasomatism: A focal plane array FTIR study from the Carpathian-Pannonian region},
	url = {https://m2.mtmt.hu/api/publication/33785006},
	author = {Liptai, Nóra and Lange, Thomas Pieter and Patkó, Levente and Aradi, László Előd and Berkesi, Márta and Peter, M. E. Tollan and José, Alberto Padrón-Navarta and Jörg, Hermann and Gergely, Szilveszter and Szabó, Csaba and Kovács, István János},
	doi = {10.2138/am-2022-8662},
	journal-iso = {AM MINERAL},
	journal = {AMERICAN MINERALOGIST},
	volume = {109},
	unique-id = {33785006},
	issn = {0003-004X},
	year = {2024},
	eissn = {1945-3027},
	pages = {87-102},
	orcid-numbers = {Liptai, Nóra/0000-0002-2464-2468; Lange, Thomas Pieter/0000-0002-8709-9239; Patkó, Levente/0000-0001-6007-3103; Aradi, László Előd/0000-0003-0276-3119; Berkesi, Márta/0000-0003-4380-057X; Gergely, Szilveszter/0000-0003-1945-526X; Szabó, Csaba/0000-0002-1580-6344; Kovács, István János/0000-0002-3488-3716}
}

@CONFERENCE{MTMT:34750002,
	title = {Deployment of a regional scale magnetotelluric (MT) array in the Pannonian Basin},
	url = {https://m2.mtmt.hu/api/publication/34750002},
	author = {Rubóczki, Tibor and Novák, Attila and Liptai, Nóra and Kovács, István János},
	booktitle = {XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) (Berlin 2023)},
	unique-id = {34750002},
	year = {2023},
	orcid-numbers = {Liptai, Nóra/0000-0002-2464-2468; Kovács, István János/0000-0002-3488-3716}
}

@misc{MTMT:34570407,
	title = {Seismicity map of the Circum-Pannonian region (456–2020) (M>2)},
	url = {https://m2.mtmt.hu/api/publication/34570407},
	author = {Győri, Erzsébet and Czecze, Barbara and Timkó, Máté and Bondár, István and Czanik, Csenge and Czifra, Tibor and Fodor, Csilla and Gráczer, Zoltán and Gribovszki, Katalin Eszter and Gyarmati, Anett and Kalmár, Dániel and Marótiné Kiszely, Márta and Kovács, István János and Mónus, Péter and Süle, Bálint and Szanyi, Gyöngyvér and Tóth, László and Varga, Péter and Zsíros, Tibor and Wéber, Zoltán},
	doi = {10.23928/foldt.kozl.2023.153.4.mapA},
	unique-id = {34570407},
	year = {2023},
	pages = {297},
	orcid-numbers = {Bondár, István/0000-0002-4892-1074; Fodor, Csilla/0000-0001-9134-4017; Gribovszki, Katalin Eszter/0000-0003-2577-0127; Kovács, István János/0000-0002-3488-3716; Wéber, Zoltán/0000-0002-0017-3505}
}

@misc{MTMT:34547257,
	title = {Tectonically Determined Distribution of Intracontinental Basaltic Volcanoes in a Compressive Tectonic Regime: A GIS Approach},
	url = {https://m2.mtmt.hu/api/publication/34547257},
	author = {Hencz, Mátyás and Biró, Tamás and Németh, Károly and Porkoláb, Kristóf and Kovács, István János and Spránitz, Tamás and Sierd, Cloetingh and Szabó, Csaba and Berkesi, Márta},
	unique-id = {34547257},
	abstract = {By analysing of spatial aspects of a monogenetic volcanic field, knowledge can be acquired on the relationships between the basaltic magmatism and regional tectonics, like impact of faults to the position of the volcanoes, vent propagation in the lithosphere, age-dependent stress condition changes. Examination of the surface patterns of volcanoes might help us understand better the process of magma generation, segregation, and how magma travelled through a thin lithosphere. Moreover, by studying these processes, we can get closer to understanding the evolution of a sedimentary basin in which we can find the link between volcanism and a changing but essentially compressive stress field, where basaltic volcanism is not evident. These spatial patterns of volcanoes can be examined using GIS (geographic information systems). The study area was the Mio-Pleistocene, monogenetic Bakony-Balaton Highland Volcanic Field (BBHVF, Carpathian-Pannonian region, Central Europe), which is located in continental back-arc setting and compressive/transpressive tectonic regime.
		The methodological toolkit included creating heatmap based on the spatial distribution of the volcanoes, measuring the orientation of the volcanic field comparing the orientation of the faults in the region, and calculating distance to the nearest fault line from each volcanic centre. Poisson nearest neighbour analysis was used to evaluate how clustered or random the occurrence of the volcanoes across the volcanic field. All volcanic lineaments (whether volcanic centres are situated along lines) were calculated, and their orientation was measured to see any systematic directions.
		The results suggest that the locations of the volcanoes in the BBHVF are most probably tectonically determined. The orientation of volcanic lineaments is also the same as the bounding geometries and the faults. Density of the volcanic centre distribution is the largest in the central area of the BBHVF along a major inactive thrust fault. We speculate that the NW dipping fault plane of this fault could be a ‘catchment area’ in the upper crust (just above the brittle-ductile transition zone), which channelized the magmas and helped them reach the surface. Volcanoes in larger distance from any faults have typically larger volume, and longer active period (several 100 ky), thus their magmas needed to have larger buoyancy to reach the surface without the help of any fault planes. Age pattern and spatial density suggest volcanism getting younger and thicker towards the central part of the BBHVF. Thus, intracontinental monogenetic volcanism in compressional regime is strongly influenced by lithospheric weaknesses and the regional stress field.},
	year = {2023},
	orcid-numbers = {Hencz, Mátyás/0000-0001-9716-5714; Biró, Tamás/0000-0001-5198-7210; Porkoláb, Kristóf/0000-0001-7470-8296; Kovács, István János/0000-0002-3488-3716; Spránitz, Tamás/0000-0002-5086-3133; Szabó, Csaba/0000-0002-1580-6344; Berkesi, Márta/0000-0003-4380-057X}
}

@book{MTMT:34542660,
	title = {Hungarian National Seismological Bulletin 2022},
	url = {https://m2.mtmt.hu/api/publication/34542660},
	author = {Czanik, Csenge and Czecze, Barbara and Czifra, Tibor and Fodor, Csilla and Gribovszki, Katalin Eszter and Gyarmati, Anett and Győri, Erzsébet and Kalmár, Dániel and Marótiné Kiszely, Márta and Kovács, István János and Timkó, Máté and Varga, Péter and Wéber, Zoltán},
	editor = {Süle, Bálint},
	publisher = {HU-REN FI Kövesligethy Radó Szeizmológiai Obszervatórium},
	unique-id = {34542660},
	year = {2023},
	orcid-numbers = {Fodor, Csilla/0000-0001-9134-4017; Gribovszki, Katalin Eszter/0000-0003-2577-0127; Kovács, István János/0000-0002-3488-3716; Wéber, Zoltán/0000-0002-0017-3505}
}

@CONFERENCE{MTMT:34521826,
	title = {Talajgáz mintavételezési módszer izotópos vizsgálatokhoz},
	url = {https://m2.mtmt.hu/api/publication/34521826},
	author = {Kővágó, Ákos and Lange, Thomas Pieter and Gelencsér, Orsolya and Palcsu, László and Szabó, Csaba and Berkesi, Márta and Kovács, István János},
	booktitle = {XXIII. Székelyföldi Geológus Találkozó konferecia kötet},
	unique-id = {34521826},
	year = {2023},
	pages = {70-71},
	orcid-numbers = {Lange, Thomas Pieter/0000-0002-8709-9239; Gelencsér, Orsolya/0000-0001-8615-9298; Szabó, Csaba/0000-0002-1580-6344; Berkesi, Márta/0000-0003-4380-057X; Kovács, István János/0000-0002-3488-3716}
}

@CONFERENCE{MTMT:34521795,
	title = {Intergrált Geodinamikai Állomások Kelet-Európában},
	url = {https://m2.mtmt.hu/api/publication/34521795},
	author = {Kovács, István János and Szabó, Csaba and Szakács, Alexandru and Lange, Thomas Pieter and Kővágó, Ákos and Gelencsér, Orsolya and Gál, Ágnes and Berkesi, Márta and Liptai, Nóra and Patkó, Levente and Gyila, Sándor and Gergely, Szilveszter and Jurdi, Dániel},
	booktitle = {XXIII. Székelyföldi Geológus Találkozó konferecia kötet},
	unique-id = {34521795},
	year = {2023},
	pages = {69-70},
	orcid-numbers = {Kovács, István János/0000-0002-3488-3716; Szabó, Csaba/0000-0002-1580-6344; Lange, Thomas Pieter/0000-0002-8709-9239; Gelencsér, Orsolya/0000-0001-8615-9298; Gál, Ágnes/0000-0001-5366-3340; Berkesi, Márta/0000-0003-4380-057X; Liptai, Nóra/0000-0002-2464-2468; Patkó, Levente/0000-0001-6007-3103; Gergely, Szilveszter/0000-0003-1945-526X}
}

@CONFERENCE{MTMT:34520313,
	title = {Hydrous nano-silicate melt inclusions in the lithospheric mantle, Persani Mountains Volcanic Field (Transylvania)},
	url = {https://m2.mtmt.hu/api/publication/34520313},
	author = {Lange, Thomas Pieter and Pálos, Zsófia and Berkesi, Márta and Pekker, Péter and Szabó, Ábel and Szabó, Csaba and Kovács, István János},
	booktitle = {Goldschmidt 2023 Conference: abstracts},
	unique-id = {34520313},
	year = {2023},
	pages = {.},
	orcid-numbers = {Lange, Thomas Pieter/0000-0002-8709-9239; Berkesi, Márta/0000-0003-4380-057X; Pekker, Péter/0000-0002-0463-0742; Szabó, Csaba/0000-0002-1580-6344; Kovács, István János/0000-0002-3488-3716}
}