@article{MTMT:1382751,
	title = {Relationship between the geometric parameters of rock fractures, the size of percolation clusters and REV},
	url = {https://m2.mtmt.hu/api/publication/1382751},
	author = {M. Tóth, Tivadar and Vass, I},
	doi = {10.1007/s11004-010-9315-4},
	journal-iso = {MATH GEOSCI},
	journal = {MATHEMATICAL GEOSCIENCES},
	volume = {43},
	unique-id = {1382751},
	issn = {1874-8961},
	year = {2011},
	eissn = {1874-8953},
	pages = {75-97},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095}
}

@article{MTMT:1436978,
	title = {Comprehensive radon concentration measurements in caves located in the area of Mecsek mountains},
	url = {https://m2.mtmt.hu/api/publication/1436978},
	author = {Koltai, Gabriella and Ország, J and Tegzes, Z and Kevei, Ferencné},
	journal-iso = {ACTA CARSOLOGICA},
	journal = {ACTA CARSOLOGICA},
	volume = {39},
	unique-id = {1436978},
	issn = {0583-6050},
	year = {2010},
	eissn = {1580-2612},
	pages = {513-522},
	orcid-numbers = {Kevei, Ferencné/0000-0002-4143-8506}
}

@article{MTMT:2092773,
	title = {Radontransport Measurements in Mecsek Mountains},
	url = {https://m2.mtmt.hu/api/publication/2092773},
	author = {Koltai, Gabriella and Ország, János and Tegzes, Zoltán and Kevei, Ferencné},
	journal-iso = {KARST DEVELOPMENT},
	journal = {KARST DEVELOPMENT},
	volume = {1},
	unique-id = {2092773},
	year = {2010},
	pages = {18-30},
	orcid-numbers = {Kevei, Ferencné/0000-0002-4143-8506}
}

@article{MTMT:1354802,
	title = {Fiatal tektonikai jelenségek új észlelései a Nyugati-Mecsekben és környezetében},
	url = {https://m2.mtmt.hu/api/publication/1354802},
	author = {Konrád, Gyula and Sebe, Krisztina},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {140},
	unique-id = {1354802},
	issn = {0015-542X},
	abstract = {Exposures of Neogene and Quaternary age were investigated along the main structural zones of the Western Mecsek
		Mts. (SW Hungary) in order to study post-Miocene tectonic activity, with an aim of supplementing studies on the longterm
		stability of the region. Field observations showed that young movements affected only the mountain fronts and the
		foreland. From the 24 studied exposures, those with impacts of tectonic activity were located along the major fault zones
		of the Western Mecsek Mts. and prove tectonic/seismic events occurring as late as the Late Pleistocene along the
		Mecsekalja Dislocation Zone and probably the Hetvehely–Magyarszék Fault. On the contrary, no impact of neotectonic
		activity was found within the Western Mecsek Anticline, indicating that this area behaved as a single solid block during
		post-Miocene movements. Since the Karpatian age, 5 tectonic phases could be distinguished. From these – somewhat
		opposing previous research – transtension seems typical for the Karpatian along the Hetvehely–Magyarszék Fault. The
		Early Pannonian transtensional stress field did not cease to exist at the beginning of the Late Pannonian. Tectonic
		inversion started only within the first half of the Late Pannonian and can be considered active up to present day in the
		major part of the area.
		
		A munka során a Nyugat-Mecsek fő szerkezeti vonalainak környezetében feltárt neogén és kvarter képződményeket
		vizsgáltuk fiatal (posztpannóniai) tektonikai aktivitás nyomai után kutatva, elsősorban a terület hosszú távú
		stabilitásának megítéléséhez. A terepi megfigyelések alapján a fiatal mozgások csak a hegységperemet és az előteret
		érintették. A vizsgált 24 feltárásból a fiatal tektonikával érintettek a Nyugat-Mecsek meghatározó szerkezeti vonalai
		mentén helyezkednek el, és még a késő-pleisztocénben is szerkezeti mozgásokat, illetve szeizmikus aktivitást
		bizonyítanak a Mecsekalja-öv és valószínűleg a Hetvehely–magyarszéki-törés mentén. Ezzel ellentétben a Nyugatmecseki-
		antiklinális területén belül neotektonikára utaló jeleket nem észleltünk, ez alapján a pannóniai–negyedidőszaki
		mozgások során a Nyugat-Mecsek egységes tömbként viselkedhetett.
		A kárpáti korszak óta öt tektonikai fázis volt elkülöníthető a területen. Ezek közül – a korábbi vizsgálati
		eredményekkel szemben – a kárpáti korszakra jellemzőnek tűnik a transztenzió a Hetvehely–magyarszéki-törés
		mentén. A kora-pannóniai transztenziós feszültségtér a Mecsekalja-öv mentén még a késő-pannóniai elején is
		fennállt. Az inverzió a késő-pannóniai első felében kezdődött és a terület legnagyobb részén máig aktívnak
		tekinthető.},
	year = {2010},
	eissn = {2559-902X},
	pages = {135-161},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199}
}

@article{MTMT:1348923,
	title = {Determination of geometric parameters of fracture networks using 1D data},
	url = {https://m2.mtmt.hu/api/publication/1348923},
	author = {M. Tóth, Tivadar},
	doi = {10.1016/j.jsg.2009.04.006},
	journal-iso = {J STRUCT GEOL},
	journal = {JOURNAL OF STRUCTURAL GEOLOGY},
	volume = {32},
	unique-id = {1348923},
	issn = {0191-8141},
	year = {2010},
	eissn = {1873-1201},
	pages = {878-885},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095}
}

@inbook{MTMT:1382869,
	title = {Az aljzati kristályos hátak szerepe az Alföld fluidum áramlási és hőtranszport folyamataiban},
	url = {https://m2.mtmt.hu/api/publication/1382869},
	author = {Vass, I and M. Tóth, Tivadar and Szanyi, János and Kovács, Balázs},
	booktitle = {Magmás és metamorf képződmények a Tiszai Egységben},
	unique-id = {1382869},
	year = {2009},
	pages = {325-339},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095; Szanyi, János/0000-0002-8053-6360}
}

@article{MTMT:1782766,
	title = {Az Abaliget orfűi karszt karsztos felszínformáinak vizsgálata térinformatikai módszerekkel},
	url = {https://m2.mtmt.hu/api/publication/1782766},
	author = {Lippmann, L. and Kiss, Klaudia and Móga, János},
	journal-iso = {KARSZTFEJLŐDÉS},
	journal = {KARSZTFEJLŐDÉS},
	volume = {13},
	unique-id = {1782766},
	issn = {1585-5473},
	year = {2008},
	pages = {151-166},
	orcid-numbers = {Móga, János/0000-0002-4471-4385}
}

@article{MTMT:1348917,
	title = {The role of neotectonics in fluvial landscape development in the Western Mecsek Mountains and related foreland basins (SE Transdanubia, Hungary)},
	url = {https://m2.mtmt.hu/api/publication/1348917},
	author = {Sebe, Krisztina and Csillag, Gábor and Konrád, Gyula},
	doi = {10.1016/j.geomorph.2007.05.018},
	journal-iso = {GEOMORPHOLOGY},
	journal = {GEOMORPHOLOGY},
	volume = {102},
	unique-id = {1348917},
	issn = {0169-555X},
	year = {2008},
	eissn = {1872-695X},
	pages = {55-67},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199}
}

@article{MTMT:1255483,
	title = {Present-day stress field and tectonic inversion in the Pannonian basin},
	url = {https://m2.mtmt.hu/api/publication/1255483},
	author = {Bada, G and Horváth, Ferenc and Dovenyi, P and Szafian, P and Windhoffer, G and Cloetingh, S},
	doi = {10.1016/j.gloplacha.2007.01.007},
	journal-iso = {GLOBAL PLANET CHANGE},
	journal = {GLOBAL AND PLANETARY CHANGE},
	volume = {58},
	unique-id = {1255483},
	issn = {0921-8181},
	abstract = {This paper presents a latest compilation of data on the present-day
		stress pattern in the Pannonian basin, and its tectonic environment,
		the Alpine-Dinaric orogens. Extensional formation of the basin system
		commenced in the early Miocene, whereas its structural reactivation, in
		the form of gradual basin inversion, has been taking place since
		Pliocene to recent times. Reconstructed compression and associated
		horizontal contraction are mainly governed by the convergence between
		Adria and its buffer, the Alpine belt of orogens. The resulting
		contemporaneous stress field exhibits important lateral variation
		resulting in a complex pattern of ongoing tectonic activity. In the
		Friuli zone of the Southern Alps, where thrust faulting prevails,
		compression is orthogonal to the strike of the mountain belt. More to
		the southeast, intense contraction is combined with active strike-slip
		faulting constituting the dextral Dinaric transpressional corridor.
		Stresses are transferred far from Adria into the Pannonian basin, and
		the dominant style of deformation gradually changes from pure
		contraction through transpression to strike-slip faulting. The
		importance of late-stage inversion in the Pannonian basin is
		interpreted in a more general context of structural reactivation of
		backarc basins where the sources of compression driving basin inversion
		are also identified and discussed. The state of recent stress and
		deformation in the Pannonian basin, particularly in its western and
		southern part, is governed by the complex interaction of plate boundary
		and intra-plate forces. The counterclockwise rotation and
		north-northeast-directed indentation of the Adriatic microplate appears
		to be of key importance as the dominant source of compression
		("Adria-push"). Intra-plate stress sources, such as buoyancy forces
		associated with an elevated topography, and crustal as well as
		lithospheric inhomogeneities can also play essential, yet rather local
		role. (C) 2007 Elsevier B.V. All rights reserved.},
	year = {2007},
	eissn = {1872-6364},
	pages = {165-180}
}

@article{MTMT:30621542,
	title = {Spatial distribution, scaling and self-similar behavior of fracture arrays in the Los Planes fault, Baja California Sur, Mexico},
	url = {https://m2.mtmt.hu/api/publication/30621542},
	author = {Nieto-Samaniego, AF and Alaniz-Alvarez, SA and Tolson, G and Oleschko, K and Korvin, Gábor and Xu, SS and Perez-Venzor, JA},
	doi = {10.1007/s00024-004-2642-y},
	journal-iso = {PURE APPL GEOPHYS},
	journal = {PURE AND APPLIED GEOPHYSICS},
	volume = {162},
	unique-id = {30621542},
	issn = {0033-4553},
	abstract = {We present a case of detailed analysis of fracture arrays spanning four orders of magnitude in length; all of them measured at a single natural site by acquiring images at progressively larger scales. There is a high dispersion of cumulative-length exponents, box dimensions and fracture densities. However, the fractal analysis supports the fractal nature of fracture arrays. Our data indicate the existence of an upper limit for the density parameters, as similarly reported by other authors. We prove that box dimension is in inverse relation with fracture concentration and in direct relation with fracture density. These relations are also observed in our data and additionally there is an upper limit for the box dimensions. We interpret the dispersion in our results as more fundamental than methodological problems. It represents a truncation in the complete evolution of the fracture systems because in natural cases strain initiates overprinting of previous fracture arrays. Considering that larger fractures accommodate strain more efficiently than small fractures, the generation of small fractures is inhibited in the presence of pre-existing larger fractures. Maximum values of fracture density prevent accommodating an excess of strain in a single or restricted range of scales; we claim this condition produces migration of fracturing to larger scales originating fracture scaling.},
	keywords = {SYSTEMS; GROWTH; LINKAGE; NETWORKS; POPULATIONS; TRANSITION; SELF-SIMILARITY; Mechanics; power-law distributions; fracture arrays; fracture density; scaling-law; BRITTLE STRAIN},
	year = {2005},
	eissn = {1420-9136},
	pages = {805-826},
	orcid-numbers = {Korvin, Gábor/0000-0003-2248-7684}
}

@article{MTMT:1129815,
	title = {Conceptual fracture network model of the crystalline basement of the Szeghalom Dome (Pannonian Basin, SE Hungary)},
	url = {https://m2.mtmt.hu/api/publication/1129815},
	author = {M. Tóth, Tivadar and Szűcs, É and Schubert, Félix and Hollós, Cs},
	doi = {10.1556/AGeol.47.2004.1.2},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {47},
	unique-id = {1129815},
	issn = {0236-5278},
	year = {2004},
	pages = {19-34},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095; Schubert, Félix/0000-0001-8647-5354}
}

@article{MTMT:2899890,
	title = {Tertiary deformation history from seismic section study and fault analysis in a former European Tethyan margin (the Mecsek-Villany area, SW Hungary)},
	url = {https://m2.mtmt.hu/api/publication/2899890},
	author = {Csontos, László and Benkovics, L and Bergerat, F and Mansy, JL and Worum, G},
	doi = {10.1016/S0040-1951(02)00363-3},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {357},
	unique-id = {2899890},
	issn = {0040-1951},
	abstract = {Outcrop-scale structural data and seismic section interpretation are combined to unveil a very complicated Tertiary deformation history of a once Tethyan margin: the Mecsek-Villany area of Hungary. This combination of data helped to reconstruct the possible activity of individual fault zones. At least four ENE-WSW striking zones-the Northern Imbricates, the South Mecsek zone, the Gorcsony-Mariakemend ridge and the Villany Mountains-were confirmed as regional long-lived transpressive zones with very complicated internal deformation, frequently with oppositely dipping thrust faults. Tertiary structural history began with a roughly N-S-directed shortening in the South Mecsek zone. It was followed by a NE-SW-directed transpression activating practically all important wrench zones together with perpendicular transfer faults. Basins were created along some of these deformation zones, but were also affected by major tilts due to inversion. After a relatively quiescent period in the Middle Miocene, the Late Sarmatian inversion followed. Shortly after, this event was relayed by a NE-SW-directed extension-transtension. An important inversion period characterised by NW-SE compression occurred in Late Pannonian (Messinian), when all the former wrench zones were reactivated as right-lateral shear. This event is responsible for the present topography of the region. (C) 2002 Elsevier Science B.V. All rights reserved.},
	year = {2002},
	eissn = {1879-3266},
	pages = {81-102}
}

@article{MTMT:1025644,
	title = {Magyarországi triász fáciesterületek szekvencia-rétegtani elemzése},
	url = {https://m2.mtmt.hu/api/publication/1025644},
	author = {Haas, János and Budai, Tamás and Hips, Kinga and Konrád, Gyula and Török, Ákos},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {132},
	unique-id = {1025644},
	issn = {0015-542X},
	year = {2002},
	eissn = {2559-902X},
	pages = {17-43},
	orcid-numbers = {Haas, János/0000-0003-0929-8889; Hips, Kinga/0000-0003-2315-120X; Török, Ákos/0000-0002-5394-4510}
}

@book{MTMT:30620625,
	title = {Fractal models in the earth sciences},
	url = {https://m2.mtmt.hu/api/publication/30620625},
	isbn = {9780444889072},
	author = {Korvin, Gábor},
	publisher = {Elsevier B.V.},
	unique-id = {30620625},
	year = {1992},
	pages = {396-792},
	orcid-numbers = {Korvin, Gábor/0000-0003-2248-7684}
}