@article{MTMT:34109504,
	title = {Integration of Geological, Geochemical Modelling and Hydrodynamic Condition for Understanding the Geometry and Flow Pattern of the Aquifer System, Southern Nyírség–Hajdúság, Hungary},
	url = {https://m2.mtmt.hu/api/publication/34109504},
	author = {Flores Carpio, Yetzabbel Gerarda and Hemida, Mohamed Hamdy Eid and Szűcs, Péter and Szőcs, Teodóra and Fancsik, Tamás and Szanyi, János and Kovács, Balázs and Markos, Gábor and Péter, Újlaki and Péter, Tóth and McIntosh, Richard William and Püspöki, Zoltán},
	doi = {10.3390/w15162888},
	journal-iso = {WATER-SUI},
	journal = {WATER},
	volume = {15},
	unique-id = {34109504},
	abstract = {Geological heterogeneity impacts groundwater flow patterns, necessitating a detailed hydrogeological framework for conceptualization process of aquifer systems. This research developed a new conceptual model of detailed geologic geometry by integrating 133 well-logs, 366 hydrodynamic data and 118 water samples. As new results, systematic 3D log correlation detected four distinct hydrostratigraphic units in the Southern Nyírség–Hajdúság Groundwater Body (East Hungary). The primary aquifer was identified as an incised valley 10–13 km wide and a NE–SW strike. Logan’s approach estimated the average hydraulic conductivity of the Incised Valley Unit (IVU) at 11 m/d, higher than the other three aquifers (3.2 m/d to 4.6 m/d). The average specific capacity of wells screening the IVU is 315.6 m3/d/m, in contrast with the remaining aquifers ranging from 31.6 m3/d/m to 92 m3/d/m. Pressure–depth profiles, dynamic pressure increment and hydraulic head maps revealed recharge–discharge zones and hydraulic windows between hydrostratigraphic units. The elongated pattern on the hydraulic head map at the depth of the IVU showed the existence of a preferential path along its axis within the mapped borders of the IVU. Hydrochemical analysis revealed Ca-Mg-HCO3 water type within the primary aquifer and Na-HCO3 water type in the laterally connected aquifer. The saturation index values indicated a transition from undersaturated to supersaturated state inside the main aquifer for calcite and dolomite minerals. The correlation matrix and PCA results demonstrated that the carbonate weathering process is the main factor controlling the groundwater chemistry. This integrated approach holds significance for future applications of the regional conceptual model in water management planning, sustainable aquifer development and contaminant transport modelling. It provides essential contributions to informed decision-making and the formulation of effective strategies, ensuring the long-term availability and utilization of groundwater resources.},
	keywords = {Conceptual model; Groundwater modeling; incised valley aquifer; geologic geometry},
	year = {2023},
	eissn = {2073-4441},
	orcid-numbers = {Flores Carpio, Yetzabbel Gerarda/0000-0003-0365-8951; Szanyi, János/0000-0002-8053-6360}
}

@article{MTMT:34015455,
	title = {Anthropic Vulnerability of a Hydrothermal Mineral Deposit and Related Mining Heritage, a Case Study from a Medieval Gold-Silver Mining Area, Telkibánya, Hungary},
	url = {https://m2.mtmt.hu/api/publication/34015455},
	author = {Szepesi, János and Sütő, László and Novák, Tibor József and Szepesi, Éva Zsuzsanna and Benkó, Zsolt and Gruber, Péter and McIntosh, Richard William and Harangi, Szabolcs and Haranginé Lukács, Réka},
	doi = {10.1007/s12371-023-00853-6},
	journal-iso = {GEOHERITAGE},
	journal = {GEOHERITAGE},
	volume = {15},
	unique-id = {34015455},
	issn = {1867-2477},
	abstract = {The movable geoheritage elements (minerals, fossils, rocks) are important part of geodiversity. Their anthropic vulnerability includes collection by geo-amateurs and professionals which has become a very popular activity in the last decades. The in situ protection of such geoheritage elements preserves their authenticity and integrity, but needs detailed inventory and assessment providing recommendation for geoconservation. The aim of this study is to investigate a medieval mining site of the Carpathians (Telkibánya, Hungary) where recent anthropic vulnerability related to mineral collecting. Earlier works emphasized the scientific, aesthetic, and geo-educational potential of the mineral association and mining heritage of the study area. Our field survey gives a review of medieval mining works and the current state of the surviving infrastructure identifies the major areas of mineral collecting disturbances and the integrity of the main and additional geological elements. Based on the degradation risk assessment, further conservation management initiatives are proposed by open collecting outcrops (exposure sites) and declared protection with controlled collecting (finite sites).},
	keywords = {VULNERABILITY; geoconservation; mining heritage; mineralogical collecting},
	year = {2023},
	eissn = {1867-2485},
	orcid-numbers = {Szepesi, János/0000-0003-1131-944X; Novák, Tibor József/0000-0002-5514-9035; Harangi, Szabolcs/0000-0003-2372-4581; Haranginé Lukács, Réka/0000-0002-2338-4209}
}

@article{MTMT:34001105,
	title = {Obliquity-driven mountain permafrost-related fluvial magnetic susceptibility cycles in the Quaternary mid-latitude long-term (2.5 Ma) fluvial Maros Fan in the Pannonian Basin},
	url = {https://m2.mtmt.hu/api/publication/34001105},
	author = {Püspöki, Zoltán and Gibbard, P.L. and Kiss, László Ferenc and McIntosh, Richard William and Thamó-Bozsó, E. and Krassay, Z. and Szappanos, B. and Maigut, V. and Kovács, Péter Gábor and Karácsony, Dominik Ádám and Stercel, F. and Visnovitz, Ferenc and Demény, K. and Bereczki, L. and Szőcs, T. and Rotár-Szalkai, Á. and Fancsik, Tamás},
	doi = {10.1111/bor.12618},
	journal-iso = {BOREAS},
	journal = {BOREAS},
	volume = {52},
	unique-id = {34001105},
	issn = {0300-9483},
	abstract = {Magnetic susceptibility (MS) of the Quaternary long-term mid-latitude Maros fluvial fan (Pannonian Basin) was
		recorded to understand the stratigraphical features of source-proximal fluvial depositional settings. Three fully cored
		500-m-deep boreholes were sampled at 0.5-m intervals; low-field and frequency dependent MS were measured, and
		complementary hysteresis and SEM-EDAX investigationswere performed on selected samples. Logged susceptibility
		data were also used to log correlations established by a simultaneous comparison of wireline log and laboratory
		measurements. Time-series analyses of the susceptibility records reveal a ∼41-ka and ∼100-ka cyclicity. Towards the
		source-distal sections the intensity of the ∼41-ka cycles decreases, while that of the ∼100-ka cycles remains strong.
		Stratigraphical and spectral similarities were observed between the Maros fluvial fan and Chinese loess records;
		however, based on complementary magnetic data, the magnetic phase of the Maros Fan sections is related to the
		detrital magnetite that originates from the catchment during early postglacial permafrost degradations. The
		amplification of the ∼41-ka cycles can be attributed to the very high susceptibility values in source-proximal settings
		and to the special stratigraphical feature of the distributive fluvial systems. This comprises the increased avulsion
		frequency on the fluvial fans in ‘glacial recession periods’, in concert with the ‘early postglacial’ occurrence of the
		permafrost-related magnetite originating from the catchment. As a local phenomenon, this is significant since it
		records the obliquity-driven variations in permafrost development in a catchment. However, fluvial and alluvial fans
		are widespread depositional landforms within the Eurasian mountain range and were possibly the same during the
		Quaternary deglaciations. Thus, obliquity-driven magnetic susceptibility variations in source-proximal fan deposits
		attached or adjacent to regions of loess deposition should also be considered when scanning for potential source
		material of aeolian deposits.},
	year = {2023},
	eissn = {1502-3885},
	pages = {402-426},
	orcid-numbers = {Visnovitz, Ferenc/0000-0002-7040-0080}
}

@article{MTMT:33072474,
	title = {Zsolcai-halmok földtudományi vizsgálata},
	url = {https://m2.mtmt.hu/api/publication/33072474},
	author = {Tóth, Csaba Albert and Pethe, Mihály and Prónay, Zsolt and McIntosh, Richard William and Novák, Tibor József and Molnár, Mihály},
	doi = {10.56617/tl.3150},
	journal-iso = {TÁJÖKOLÓGIAI LAPOK / J LANDSCAPE ECOL},
	journal = {TÁJÖKOLÓGIAI LAPOK / JOURNAL OF LANDSCAPE ECOLOGY},
	volume = {20},
	unique-id = {33072474},
	issn = {1589-4673},
	abstract = {Az Alföld északi részén, a Sajó ármentes teraszán emelkedő, 6 méter magas, régészetileg feltáratlan kettős halom vizsgálata volt a célunk, mivel korábban szinte semmilyen kutatás nem zajlott e halmokkal kapcsolatban. Ha egyenként vizsgáljuk e halmokat, akkor a közepes, átlagos méretű hazai halmok csoportjába tartoznak. Az viszont már egyáltalán nem tekinthető magyarországi viszonylatban átlagosnak, hogy két, tájképileg és növénytakaróját tekintve kiemelkedően értékes, szorosan egymás mellé épült prehisztorikus halom mai napig fennmaradt egy intenzíven átalakított kultúrtájban. A rétegtani és kőzettani elemzések alapján a Zsolcai-halmok fő építőanyaga a közeli Bükkből származó mészkő, a Szerencsi-dombságból bányászott riolittufa, a halmok lábánál kitermelt termőtalaj és talajjal kevert sárgásbarna pleisztocén löszös üledék. Mindkét halmot fél méternél nem mélyebb, gyűrűszerű mélyedés vesz körbe jelenleg, amelyek eredetileg közel három méter mély, talajvízzel töltött árkok lehettek. Ezekből termelhették ki a halomtestek magasításához szükséges építőanyagot. Az eltemetett paleotalajok radiokarbon kora alapján (cal BC 950–404 és cal BC 879–542) kijelenthető, hogy a két halom az i.e. 9-6. században épülhetett szinte teljesen egyidőben. A geoelektromos, radiokarbon és kőzettani vizsgálatok alapján épített sírkamrával rendelkező szkíta kurgánnak határoztuk meg a kettős halmot. A mágneses anomália mérések szerint a halmoktól északra elterülő sík térszínen több szarmata körárkos sírt azonosítottunk. Mindez azt bizonyítja, hogy a Zsolcai-halmok az időszámításunk utáni 4. évszázadban is fontos kultikus, szakrális helyszínek voltak.},
	keywords = {PALEOSOLS; kurgan; Habitat islands; talaj-és kőzetelemzés; geofizikai vizsgálatok; radiokarbon kormeghatározás; eltemetett talajok; élőhelyszigetek; soil and petrological analyses; geophysical analyses; radiocarbon age determination},
	year = {2022},
	pages = {63-89},
	orcid-numbers = {Novák, Tibor József/0000-0002-5514-9035}
}

@article{MTMT:32751175,
	title = {Subregion-Scale Geothermal Delineation Based on Image Analysis Using Reflection Seismology and Well Data with an Outlook for Land Use},
	url = {https://m2.mtmt.hu/api/publication/32751175},
	author = {Budayné Bódi, Erika and Irfan, Ali and McIntosh, Richard William and Fehér, Zsolt Zoltán and Csajbók, József and Juhász, Csaba and Radócz, László and Szilágyi, Arnold and Buday, Tamás},
	doi = {10.3390/su14063529},
	journal-iso = {SUSTAINABILITY-BASEL},
	journal = {SUSTAINABILITY},
	volume = {14},
	unique-id = {32751175},
	abstract = {The role of geothermal energy is smaller in the global energy mix than what its potential would indicate, but it can be improved by incorporating geothermal energy potential assessments into spatial planning. For adequate decision support and sustainable utilisation, subregion-scale assessments should be applied due to the high variability in geothermal characteristics. Different GIS tools were used for the interpretation and integration of the different spatial data into one model showing areas with their geothermal characteristics on maps. Considering the present study site with a size of 83 km × 103 km located in NE Hungary, 39 2D reflection seismic sections and high-resolution geological data of 137 thermal wells were interpreted in OpendTect and then in ArcGIS to define spatial differences in geothermal potential. It was found that nine geothermal subregions (GSRs) can be distinguished in the present study site based on the applied GIS algorithms. Each GSR was characterised and land-use structure was studied based on Corine Land Cover 2018. The exploitation of water with at least 30 °C is possible in all GSRs, while the maximum achievable temperature and reservoir geometry vary; a subregion-scale delineation framework is required for regional planning.},
	keywords = {GIS tools; reflection seismic interpretation; geothermal subregions; Corine Land Cover 2018},
	year = {2022},
	eissn = {2071-1050},
	orcid-numbers = {Csajbók, József/0000-0003-0281-2590}
}

@inbook{MTMT:32524033,
	title = {Magyarországi díszítőkövek szilárdsági és hővezetőképességi tulajdonságainak roncsolásmentes vizsgálata},
	url = {https://m2.mtmt.hu/api/publication/32524033},
	author = {McIntosh, Richard William and Buday, Tamás and Varga, Gábor},
	booktitle = {Műszaki Tudomány az Észak-kelet Magyarországi Régióban 2021 Konferencia},
	unique-id = {32524033},
	abstract = {Magyarországi, díszítőkőként is használható kőzetminták szilárdsági és hővezetési tulajdonságait vizsgáltuk RockSchmidt L kalapáccsal és Hukseflux TP01 lapszenzor segítségével. Mindkét tulajdonság a minták testsűrűségével pozitív korrelációban van, és a két érték több kőzettípus esetén egymással is korrelál. A mért értékek és megállapított összefüggések felhasználhatók az építőiparban és a műemlékvédelemben.},
	keywords = {hővezetési tényező; RockSchmidt L; testsűrűség; díszítőkövek; mészkő},
	year = {2021},
	pages = {19-22}
}

@{MTMT:32524032,
	title = {Magyarországi díszítőkövek szilárdsági és hővezetőképességi tulajdonságainak roncsolásmentes vizsgálata},
	url = {https://m2.mtmt.hu/api/publication/32524032},
	author = {McIntosh, Richard William and Buday, Tamás and Varga, Gábor},
	booktitle = {Műszaki Tudomány az Észak-kelet Magyarországi Régióban 2021},
	unique-id = {32524032},
	keywords = {hővezetési tényező; kőzet; Schmidt kalapács},
	year = {2021},
	pages = {45-46}
}

@{MTMT:32524031,
	title = {Kőzeteken végzett hővezetési tényező mérések reprezentativitása},
	url = {https://m2.mtmt.hu/api/publication/32524031},
	author = {Buday, Tamás and McIntosh, Richard William},
	booktitle = {Műszaki Tudomány az Észak-kelet Magyarországi Régióban 2021},
	unique-id = {32524031},
	keywords = {hővezetési tényező; kőzet},
	year = {2021},
	pages = {38}
}

@article{MTMT:31950068,
	title = {Fluvial magnetic susceptibility as a proxy for long‐term variations of mountain permafrost development in the Alp‐Carpathian region},
	url = {https://m2.mtmt.hu/api/publication/31950068},
	author = {Püspöki, Zoltán and Gibbard, PL and Nádor, A and Thamóné Bozsó, Edit and Sümegi, Pál and Fogarassy-Pummer, Tímea and McIntosh, Richard William and Lantos, M and Tóth‐Makk, Á and Stercel, F and Krassay, Z and Kovács, Péter Gábor and Szőcs, Teodóra and Fancsik, Tamás},
	doi = {10.1111/bor.12520},
	journal-iso = {BOREAS},
	journal = {BOREAS},
	volume = {50},
	unique-id = {31950068},
	issn = {0300-9483},
	keywords = {földtan},
	year = {2021},
	eissn = {1502-3885},
	pages = {806-825},
	orcid-numbers = {Püspöki, Zoltán/0000-0002-8282-7620; Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:31621407,
	title = {High‐resolution stratigraphy of Quaternary fluvial deposits in the Makó Trough and the Danube‐Tisza Interfluve, Hungary, based on magnetic susceptibility data},
	url = {https://m2.mtmt.hu/api/publication/31621407},
	author = {Püspöki, Zoltán and Fogarassy-Pummer, Tímea and Thamóné Bozsó, Edit and Falus, György and Cserkész-Nagy, Ágnes and Szappanos, B and Márton Péterné Szalay, Emőke and Lantos, Zoltán and Szabó, Szilárd and Stercel, F and Tóth‐Makk, Á and McIntosh, Richard William and Szőcs, Teodóra and Pálóczy, P and Fancsik, Tamás},
	doi = {10.1111/bor.12471},
	journal-iso = {BOREAS},
	journal = {BOREAS},
	volume = {50},
	unique-id = {31621407},
	issn = {0300-9483},
	keywords = {Duna-Tisza köze; földtan},
	year = {2021},
	eissn = {1502-3885},
	pages = {205-223},
	orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867; Szabó, Szilárd/0000-0002-2670-7384}
}