@article{MTMT:31168881,
	title = {New methods of geothermal potential assessment in the Pannonian basin},
	url = {https://m2.mtmt.hu/api/publication/31168881},
	author = {Nádor, Annamária and Sebess-Zilahi, László and Rotárné Szalkai, Ágnes and Gulyás, Ágnes and Markovic, Tamara},
	doi = {10.1017/njg.2019.7},
	journal-iso = {NETH J GEOSCI},
	journal = {NETHERLANDS JOURNAL OF GEOSCIENCES-GEOLOGIE EN MIJNBOUW},
	volume = {98},
	unique-id = {31168881},
	issn = {0016-7746},
	year = {2020},
	eissn = {1573-9708},
	orcid-numbers = {Nádor, Annamária/0000-0002-2454-5756}
}

@article{MTMT:3240055,
	title = {Confined carbonates–Regional scale hydraulic interaction or isolation?},
	url = {https://m2.mtmt.hu/api/publication/3240055},
	author = {Mádlné Szőnyi, Judit and Czauner, Brigitta and Iván, Veronika and Tóth, Ádám and Simon, Szilvia and Erőss, Anita and Kovácsné Bodor, Petra and Trásy-Havril, Tímea and Boncz, László and Sőreg, Viktor},
	doi = {10.1016/j.marpetgeo.2017.06.006},
	journal-iso = {MAR PETROL GEOL},
	journal = {MARINE AND PETROLEUM GEOLOGY},
	volume = {107},
	unique-id = {3240055},
	issn = {0264-8172},
	year = {2019},
	eissn = {1873-4073},
	pages = {591-612},
	orcid-numbers = {Mádlné Szőnyi, Judit/0000-0002-5628-4386; Czauner, Brigitta/0000-0001-6591-8611; Tóth, Ádám/0000-0002-7300-6687; Simon, Szilvia/0000-0002-3811-9141; Erőss, Anita/0000-0002-2395-3934; Trásy-Havril, Tímea/0000-0003-3478-2787}
}

@article{MTMT:31131532,
	title = {Geothermal sources and utilization practice in six countries along the southern part of the Pannonian basin},
	url = {https://m2.mtmt.hu/api/publication/31131532},
	author = {Rman, Nina and Bălan, Lidia-Lenuța and Bobovečki, Ivana and Gál, Nóra Edit and Jolović, Boban and Lapanje, Andrej and Marković, Tamara and Milenić, Dejan and Skopljak, Ferid and Rotárné Szalkai, Ágnes and Samardžić, Natalija and Szőcs, Teodóra and Šolaja, Dragana and Toholj, Nenad and Vijdea, Anca-Marina and Vranješ, Ana},
	doi = {10.1007/s12665-019-8746-6},
	journal-iso = {ENVIRON EARTH SCI},
	journal = {ENVIRONMENTAL EARTH SCIENCES},
	volume = {79},
	unique-id = {31131532},
	issn = {1866-6280},
	year = {2019},
	eissn = {1866-6299}
}

@article{MTMT:30573099,
	title = {Numerical investigation of the combined effect of forced and free thermal convection in synthetic groundwater basins},
	url = {https://m2.mtmt.hu/api/publication/30573099},
	author = {Szijártó, Márk and Galsa, Attila and Tóth, Ádám and Mádlné Szőnyi, Judit},
	doi = {10.1016/j.jhydrol.2019.03.003},
	journal-iso = {J HYDROL},
	journal = {JOURNAL OF HYDROLOGY},
	volume = {572},
	unique-id = {30573099},
	issn = {0022-1694},
	abstract = {The theoretical examination of the combined effect of water table configuration and heat transfer is relevant to improve understanding of deep groundwater systems, not only in siliciclastic sedimentary basins, but also in fractured rocks or karstified carbonates. Numerical model calculations have been carried out to investigate the interaction of topography-driven forced and buoyancy-driven free thermal convection in a synthetic, two-dimensional model. Effects of numerous model parameters were systematically studied in order to examine their influence on the Darcy flux, the temperature and the hydraulic head field. It was established that higher geothermal gradients and greater model depths facilitate the evolution of time-dependent free thermal convection in agreement with changes of the thermal Rayleigh number and the modified Péclet number. However, increasing water table slope and anisotropy coefficient favor the formation of stationary forced thermal convection. Free thermal convection mainly affects the deeper part of the midline and the discharge zone of the synthetic model. In the examined model basins, the position of the maximum hydraulic head is located within the bottom thermal boundary layer near the recharge zone. This divergent stagnation point underlies a local downwelling zone characterized by underpressure. These simulations draw attention to the importance of understanding the combined effect of forced and free thermal convection in sedimentary basins regarding regional groundwater flow patterns, and temperature distributions.},
	keywords = {Finite element numerical modeling; heat transport; topography-driven groundwater flow; thermal buoyancy; forced and free thermal convection},
	year = {2019},
	eissn = {1879-2707},
	pages = {364-379},
	orcid-numbers = {Szijártó, Márk/0000-0001-5408-4092; Galsa, Attila/0000-0002-7198-4524; Tóth, Ádám/0000-0002-7300-6687; Mádlné Szőnyi, Judit/0000-0002-5628-4386}
}

@mastersthesis{MTMT:30599840,
	title = {A Balaton-felvidék felszínalatti vizeinek hidraulikai kapcsolata a Bakonnyal és a Balatonnal},
	url = {https://m2.mtmt.hu/api/publication/30599840},
	author = {Tóth, Ádám},
	doi = {10.15476/ELTE.2018.123},
	publisher = {Eötvös Loránd University},
	unique-id = {30599840},
	year = {2019},
	orcid-numbers = {Tóth, Ádám/0000-0002-7300-6687}
}

@article{MTMT:26902707,
	title = {Subsurface temperature model of the Hungarian part of the Pannonian Basin},
	url = {https://m2.mtmt.hu/api/publication/26902707},
	author = {Békési, Eszter and Lenkey, László and Limberger, J and Porkoláb, Kristóf and Balázs, Attila and Bonté, D and Vrijlandt, M and Horváth, Ferenc and Cloetingh, S and van Wees, JD},
	doi = {10.1016/j.gloplacha.2017.09.020},
	journal-iso = {GLOBAL PLANET CHANGE},
	journal = {GLOBAL AND PLANETARY CHANGE},
	volume = {171},
	unique-id = {26902707},
	issn = {0921-8181},
	abstract = {Hungary is one of the most suitable countries in Europe for geothermal development, as a result of large amounts of Miocene extension and associated thermal attenuation of the lithosphere. For geothermal exploration, it is crucial to have an insight into the subsurface temperature distribution. A new thermal model of Hungary is presented extending from the surface down to the lithosphere-asthenosphere boundary (LAB) based on a new stochastic thermal modeling workflow. The model solves the heat equation in steady-state, assuming conduction as the main heat transfer mechanism. At the top and the base, we adopt a constant surface temperature and basal heat flow condition. For the calibration of the model, temperature measurements were collected from the Geothermal Database of Hungary. The model is built up in a layered structure, where each layer has its own thermal properties. The prior thermal properties and basal condition of the model are updated through the ensemble smoother with multiple data assimilation technique. The prior model shows a misfit with the observed temperatures, which is explained fundamentally by transient thermal effects and non-conductive heat transfer. Other misfits can be attributed to a-priori assumptions on thermal properties, boundary conditions, and uncertainty in the model geometry. The updated models considerably improve the prior model, showing a better fit with measured records. The updated models are capable to reproduce the thermal effect of lithospheric extension and the sedimentary infill of the Pannonian Basin. Results indicate that the hottest areas below 3 km are linked to the basement highs surrounded by deep subbasins of the Great Hungarian Plain. Our models provide an indication on the potential sites for future EGS in Hungary and can serve as an input for geothermal resource assessment.},
	keywords = {EVOLUTION; Neogene; Tectonics; continental lithosphere; STRUCTURAL-ANALYSIS; Quaternary volcanism; Back-arc basins; HEAT-FLOW; Geography, Physical; TRANSDANUBIAN RANGE HUNGARY},
	year = {2018},
	eissn = {1872-6364},
	pages = {48-64},
	orcid-numbers = {Békési, Eszter/0000-0003-3561-1656; Lenkey, László/0000-0003-4236-4075; Porkoláb, Kristóf/0000-0001-7470-8296; Balázs, Attila/0000-0003-2948-0397}
}

@article{MTMT:3334252,
	title = {Lithospheric scale 3D thermal model of the Alpine–Pannonian transition zone},
	url = {https://m2.mtmt.hu/api/publication/3334252},
	author = {Lenkey, László and Raáb, D and Goetzl, G and Lapanje, A and Nádor, Annamária and Rajver, D and Rotárné Szalkai, Ágnes and Svasta, J and Zekiri, F},
	doi = {10.1007/s40328-017-0194-8},
	journal-iso = {ACTA GEOD GEOPHYS},
	journal = {ACTA GEODAETICA ET GEOPHYSICA},
	volume = {52},
	unique-id = {3334252},
	issn = {2213-5812},
	year = {2017},
	eissn = {2213-5820},
	pages = {161-182},
	orcid-numbers = {Lenkey, László/0000-0003-4236-4075}
}

@article{MTMT:3330762,
	title = {Outline and joint characterization of Transboundary geothermal reservoirs at the western part of the Pannonian basin},
	url = {https://m2.mtmt.hu/api/publication/3330762},
	author = {Rotárné Szalkai, Ágnes and Nádor, Annamária and Szőcs, Teodóra and Maros, Gyula and GOETZL, G and ZEKIRI, F},
	doi = {10.1016/j.geothermics.2017.05.005},
	journal-iso = {GEOTHERMICS},
	journal = {GEOTHERMICS},
	volume = {70},
	unique-id = {3330762},
	issn = {0375-6505},
	year = {2017},
	eissn = {1879-3576},
	pages = {1-16},
	orcid-numbers = {Maros, Gyula/0000-0002-2973-4513}
}

@article{MTMT:3001560,
	title = {Involvement of preliminary regional fluid pressure evaluation into the reconnaissance geothermal exploration—Example of an overpressured and gravity-driven basin},
	url = {https://m2.mtmt.hu/api/publication/3001560},
	author = {Mádlné Szőnyi, Judit and Simon, Szilvia},
	doi = {10.1016/j.geothermics.2015.11.001},
	journal-iso = {GEOTHERMICS},
	journal = {GEOTHERMICS},
	volume = {60},
	unique-id = {3001560},
	issn = {0375-6505},
	year = {2016},
	eissn = {1879-3576},
	pages = {156-174},
	orcid-numbers = {Mádlné Szőnyi, Judit/0000-0002-5628-4386; Simon, Szilvia/0000-0002-3811-9141}
}

@article{MTMT:3033376,
	title = {Transboundary fresh and thermal groundwater flows in the west part of thePannonian Basin},
	url = {https://m2.mtmt.hu/api/publication/3033376},
	author = {Tóth, György and Rotárné Szalkai, Ágnes and Kerékgyártó, Tamás and Szőcs, Teodóra and Lapanje, A and Černák, R and Remsík, A and Schubert, G and Nádor, Annamária and Rman, M.},
	doi = {10.1016/j.rser.2015.12.021},
	journal-iso = {RENEW SUST ENERG REV},
	journal = {RENEWABLE & SUSTAINABLE ENERGY REVIEWS},
	volume = {57},
	unique-id = {3033376},
	issn = {1364-0321},
	year = {2016},
	eissn = {1879-0690},
	pages = {439-454}
}

@article{MTMT:2719067,
	title = {Evolution of the Pannonian basin and its geothermal resources},
	url = {https://m2.mtmt.hu/api/publication/2719067},
	author = {Horváth, Ferenc and Musitz, Balázs and Balázs, Attila and Végh, Andor and Uhrin, András and Nádor, Annamária and Koroknai, B and Pap, Norbert and Tóth, Tamás and Wórum, G},
	doi = {10.1016/j.geothermics.2014.07.009},
	journal-iso = {GEOTHERMICS},
	journal = {GEOTHERMICS},
	volume = {53},
	unique-id = {2719067},
	issn = {0375-6505},
	keywords = {Pannonian Basin; Tectonics; Geothermal installations; Thermal water reservoirs},
	year = {2015},
	eissn = {1879-3576},
	pages = {328-352},
	orcid-numbers = {Balázs, Attila/0000-0003-2948-0397; Pap, Norbert/0000-0001-8243-4213}
}

@article{MTMT:2969005,
	title = {Basin-scale conceptual groundwater flow model for an unconfined and confined thick carbonate region},
	url = {https://m2.mtmt.hu/api/publication/2969005},
	author = {Mádlné Szőnyi, Judit and Tóth, Ádám},
	doi = {10.1007/s10040-015-1274-x},
	journal-iso = {HYDROGEOL J},
	journal = {HYDROGEOLOGY JOURNAL},
	volume = {23},
	unique-id = {2969005},
	issn = {1431-2174},
	abstract = {Application of the gravity-driven regional groundwater flow (GDRGF) concept to the hydrogeologically complex thick carbonate system of the Transdanubian Range (TR), Hungary, is justified based on the principle of hydraulic continuity. The GDRGF concept informs about basin hydraulics and groundwater as a geologic agent. It became obvious that the effect of heterogeneity and anisotropy on the flow pattern could be derived from hydraulic reactions of the aquifer system. The topography and heat as driving forces were examined by numerical simulations of flow and heat transport. Evaluation of groups of springs, in terms of related discharge phenomena and regional chloride distribution, reveals the dominance of topography-driven flow when considering flow and related chemical and temperature patterns. Moreover, heat accumulation beneath the confined part of the system also influences these patterns. The presence of cold, lukewarm and thermal springs and related wetlands, creeks, mineral precipitates, and epigenic and hypogenic caves validates the existence of GDRGF in the system. Vice versa, groups of springs reflect rock–water interaction and advective heat transport and inform about basin hydraulics. Based on these findings, a generalized conceptual GDRGF model is proposed for an unconfined and confined carbonate region. An interface was revealed close to the margin of the unconfined and confined carbonates, determined by the GDRGF and freshwater and basinal fluids involved. The application of this model provides a background to interpret manifestations of flowing groundwater in thick carbonates generally, including porosity enlargement and hydrocarbon and heat accumulation. © 2015, Springer-Verlag Berlin Heidelberg.},
	keywords = {Hungary; groundwater flow; Hydraulic properties; Carbonate rocks; Geological agency},
	year = {2015},
	eissn = {1435-0157},
	pages = {1359-1380},
	orcid-numbers = {Mádlné Szőnyi, Judit/0000-0002-5628-4386; Tóth, Ádám/0000-0002-7300-6687}
}

@article{MTMT:3033346,
	title = {Potentials of transboundary thermal water resources in the western part of the Pannonian basin},
	url = {https://m2.mtmt.hu/api/publication/3033346},
	author = {Rman, N and Gál, Nóra Edit and Marcin, D and Weibold, J and Schubert, J and Lapanje, A and Rajver, D and Benková, K and Nádor, Annamária},
	doi = {10.1016/j.geothermics.2015.01.013},
	journal-iso = {GEOTHERMICS},
	journal = {GEOTHERMICS},
	volume = {55},
	unique-id = {3033346},
	issn = {0375-6505},
	year = {2015},
	eissn = {1879-3576},
	pages = {88-98}
}

@book{MTMT:2048748,
	title = {Geology of Hungary},
	url = {https://m2.mtmt.hu/api/publication/2048748},
	isbn = {9783642219092},
	doi = {10.1007/978-3-642-21910-8},
	editor = {Haas, János},
	publisher = {Springer Netherlands},
	unique-id = {2048748},
	year = {2013},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@article{MTMT:1441814,
	title = {Lithosphere tectonics and thermo-mechanical properties: An integrated modelling approach for Enhanced Geothermal Systems exploration in Europe},
	url = {https://m2.mtmt.hu/api/publication/1441814},
	author = {Cloetingh, S and van Wees, JD and Ziegler, PA and Lenkey, László and Beekman, F and Tesauro, M and Förster, A and Norden, B and Kaban, M and Hardebol, N and Bonté, D and Genter, A and Guillou-Frottier, L and Ter, Voorde M and Sokoutis, D and Willingshofer, E and Cornu, T and Worum, G},
	doi = {10.1016/j.earscirev.2010.05.003},
	journal-iso = {EARTH-SCI REV},
	journal = {EARTH-SCIENCE REVIEWS},
	volume = {102},
	unique-id = {1441814},
	issn = {0012-8252},
	year = {2010},
	eissn = {1872-6828},
	pages = {159-206},
	orcid-numbers = {Lenkey, László/0000-0003-4236-4075}
}

@book{MTMT:2947371,
	title = {Gravitational systems of groundwater flow},
	url = {https://m2.mtmt.hu/api/publication/2947371},
	isbn = {9780511576546},
	author = {Tóth, József},
	doi = {10.1017/CBO9780511576546},
	publisher = {Cambridge University Press & Assessment},
	unique-id = {2947371},
	abstract = {This book recognises groundwater flow as a fundamental geologic agent, and presents a wide-ranging and illustrated overview of its history, principles, scientific consequences and practical utilization. The author, one of the founding fathers of modern hydrogeology, highlights key interrelationships between seemingly disparate processes and systems by tracing them to a common root cause - gravity-driven groundwater flow. Numerous examples demonstrate practical applications in a diverse range of subjects, including land-use planning, environment protection, wetland ecology, agriculture, forestry, geotechnical engineering, nuclear-waste disposal, mineral and petroleum exploration, and geothermal heat flow. The book contains numerous user-friendly features for a multidisciplinary readership, including full explanations of the relevant mathematics, emphasis on the physical meaning of the equations, and an extensive glossary. It is a key reference for researchers, consultants and advanced students of hydrogeology and reservoir engineering. © J. Tóth 2009 and Cambridge University Press, 2009. All rights reserved.},
	year = {2009}
}

@article{MTMT:2176402,
	title = {Formation and deformation of the Pannonian Basin: Constraints from observational data},
	url = {https://m2.mtmt.hu/api/publication/2176402},
	isbn = {1862392129},
	author = {Horváth, Ferenc and Bada, G and Szafián, P and Tari, Gábor and Ádám, A and Cloetingh, S},
	doi = {10.1144/GSL.MEM.2006.032.01.11},
	journal-iso = {MEM GEOL SOC LOND},
	journal = {MEMOIRS OF THE GEOLOGICAL SOCIETY OF LONDON},
	volume = {32},
	unique-id = {2176402},
	issn = {0435-4052},
	abstract = {The past decade has witnessed spectacular progress in the collection of observational data and their interpretation in the Pannonian Basin and the surrounding Alpine, Carpathian and Dinaric mountain belts. A major driving force behind this progress was the PANCARDI project of the EUROPROBE programme. The paper reviews tectonic processes, structural styles, stratigraphic records and geochemical data for volcanic rocks. Structural and seismic sections of different scales, seismic tomography and magnetotelluric, gravity and geothermal data are also used to determine the deformational styles, and to compile new crustal and lithospheric thickness maps of the Pannonian Basin and the surrounding fold-and-thrust belts. The Pannonian Basin is superimposed on former Alpine terranes. Its formation is a result of extensional collapse of the overthickened Alpine orogenic wedge during orogen-parallel extrusion towards a 'free boundary' offered by the roll-back of the subducting Carpathian slab, As a conclusion, continental collision and back-arc basin evolution is discussed as a single, complex dynamic process, with minimization of the potential and deformational energy as the driving principle. © The Geological Society of London 2006.},
	keywords = {Europe; Eurasia; extrusion; SUBDUCTION; Pannonian Basin; continental collision; orogeny; basin evolution; Formation mechanism; deformation mechanism; fold and thrust belt; backarc basin; tectonic wedge},
	year = {2006},
	eissn = {2041-4722},
	pages = {191-206}
}

@article{MTMT:1236932,
	title = {Mesozoic plate tectonic reconstruction of the carpathian region},
	url = {https://m2.mtmt.hu/api/publication/1236932},
	author = {Csontos, L and Vörös, Attila},
	doi = {10.1016/j.palaeo.2004.02.033},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {210},
	unique-id = {1236932},
	issn = {0031-0182},
	abstract = {Palaeomagnetic, palaeobiogeographic and structural comparisons of
		different parts of the Alpine-Carpathian region suggest that four
		terranes comprise this area: the Alcapa, Tisza, Dacia and Adria
		terranes. These terranes are composed of different Mesozoic continental
		and oceanic fragments that were each assembled during a complex Late
		Jurassic-Cretaceous Palaeogene history. Palaeomagnetic and tectonic
		data suggest that the Carpathians are built up by two major oroclinal
		bends. The Alcapa bend has the Meliata oceanic unit, correlated with
		the Dinaric Vardar ophiolite, in its core. It is composed of the
		Western Carpathians, Eastern Alps and Southern Alcapa units
		(Transdanubian Range, Bukk). This terrane finds its continuation in the
		High Karst margin of the Dinarides. Further elements of the Alcapa
		terrane are thought to be derived from collided microcontinents:
		Czorsztyn in the N and a carbonate unit (Tisza?) in the SE. The
		Tisza-Dacia bend has the Vardar oceanic unit in its core. It is
		composed of the Bihor and Getic microcontinents. This terrane finds its
		continuation in the Serbo-Macedonian Massif of the Balkans.
		The Bihor-Getic microcontinent originally laid east of the Western
		Carpathians and filled the present Carpathian embayment in the Late
		Palaeozoic-Early Mesozoic. The Vardar ocean occupied an intermediate
		position between the Western Carpathian-Austroalpine-Transdanubian-High
		Karst margin and the Bihor-Getic-Serbo-Macedonian microcontinent. The
		Vardar and Pindos oceans were opened in the heart of the
		Mediterranean-Adriatic microcontinent in the Late Permian-Middle
		Triassic. Vardar subducted by the end of Jurassic, causing the
		Bihor-Getic-Serbo-Macedonian microcontinent to collide with the
		internal Dinaric-Western Carpathian margin.
		An external Penninic-Vahic ocean tract began opening in the Early
		Jurassic, separating the Austroalpine-Western Carpathian microcontinent
		(and its fauna) from the European shelf. Further east, the
		Severin-Ceahlau-Magura also began opening in the Early Jurassic, but
		final separation of the Bihor-Getic ribbon (and its fauna) from the
		European shelf did not take place until the late Middle Jurassic.
		The Alcapa and the Tisza-Dacia were bending during the
		Albian-Maastrichtian. The two oroclinal bends were finally opposed and
		pushed into the gates of the Carpathian embayment during the Palaeogene
		and Neogene. At that time, the main NS shortening in distant Alpine and
		Hellenic sectors was linked by a broader right-lateral shear zone along
		the former Vardar suture. (C) 2004 Elsevier B.V. All rights reserved.},
	year = {2004},
	eissn = {1872-616X},
	pages = {1-56}
}

@article{MTMT:2947090,
	title = {Groundwater as a geologic agent: An overview of the causes, processes, and manifestations},
	url = {https://m2.mtmt.hu/api/publication/2947090},
	author = {Tóth, József},
	doi = {10.1007/s100400050176},
	journal-iso = {HYDROGEOL J},
	journal = {HYDROGEOLOGY JOURNAL},
	volume = {7},
	unique-id = {2947090},
	issn = {1431-2174},
	abstract = {The objective of the present paper is to show that groundwater is a general geologic agent. This perception could not, and did not, evolve until the system nature of basinal groundwater flow and its properties, geometries, and controlling factors became recognized and understood through the 1960s and 1970s. The two fundamental causes for groundwater's active role in nature are its ability to interact with the ambient environment and the systematized spatial distribution of its flow. Interaction and flow occur simultaneously at all scales of space and time, although at correspondingly varying rates and intensities. Thus, effects of groundwater flow are created from the land surface to the greatest depths of the porous parts of the Earth's crust, and from a day's length through geologic times. Three main types of interaction between groundwater and environment are identified in this paper, with several special processes for each one, namely: (1) Chemical interaction, with processes of dissolution, hydration, hydrolysis, oxidation-reduction, attack by acids, chemical precipitation, base exchange, sulfate reduction, concentration, and ultrafiltration or osmosis; (2) Physical interaction, with processes of lubrication and pore-pressure modification; and (3) Kinetic interaction, with the transport processes of water, aqueous and nonaqueous matter, and heat. Owing to the transporting ability and spatial patterns of basinal flow, the effects of interaction are cumulative and distributed according to the geometries of the flow systems. The number and diversity of natural phenomena that are generated by groundwater flow are almost unlimited, due to the fact that the relatively few basic types are modified by some or all of the three components of the hydrogeologic environment: topography, geology, and climate. The six basic groups into which manifestations of groundwater flow have been divided are: (1) Hydrology and hydraulics; (2) Chemistry and mineralogy; (3) Vegetation; (4) Soil and rock mechanics; (5) Geomorphology; and (6) Transport and accumulation. Based on such a diversity of effects and manifestations, it is concluded that groundwater is a general geologic agent.},
	year = {1999},
	eissn = {1435-0157},
	pages = {1-14}
}

@article{MTMT:2947300,
	title = {PETROLEUM HYDROGEOLOGY - A POTENTIAL APPLICATION OF GROUNDWATER SCIENCE},
	url = {https://m2.mtmt.hu/api/publication/2947300},
	author = {Tóth, József},
	journal-iso = {J GEOL SOC INDIA},
	journal = {JOURNAL OF THE GEOLOGICAL SOCIETY OF INDIA},
	volume = {29},
	unique-id = {2947300},
	issn = {0016-7622},
	year = {1987},
	eissn = {0974-6889},
	pages = {172-179}
}