@inproceedings{MTMT:33273243,
	title = {A Mecsekalja-zóna Au-Ag-Bi-Te ércesedésének felfedezése.},
	url = {https://m2.mtmt.hu/api/publication/33273243},
	author = {Jáger, Viktor and Molnár, Ferenc and Király, Edit and Palotai, Márton and Török, Kálmán},
	booktitle = {Calce et malleo – Mésszel és kalapáccsal},
	unique-id = {33273243},
	year = {2022},
	pages = {58-60},
	orcid-numbers = {Jáger, Viktor/0000-0003-1283-5198; Molnár, Ferenc/0000-0002-1873-1915}
}

@article{MTMT:33632115,
	title = {Nemesfémkutatások a Kelet-Mecsekben: egy új orogén aranyércesedés felfedezése a Mecsekalja-zónában.},
	url = {https://m2.mtmt.hu/api/publication/33632115},
	author = {Jáger, Viktor and Molnár, Ferenc and Király, Edit},
	doi = {10.23928/foldt.kozl.2022.152.4.307},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {152},
	unique-id = {33632115},
	issn = {0015-542X},
	abstract = {A török kiűzését követően, a 17–18. század fordulóján a Mecsek környéki településeken is megjelentek az ipari tevékenységekben jártas németajkú telepesek, akik a Mecsek erdeiben az első üveghuták létesítési munkálatai közben felfigyeltek a környék ércindikációira is. Levéltári dokumentumok igazolják ezeket a nemesfémkutatásokat, azonban mindezidáig tényfeltáró és a történeti kutatásokat összefoglaló munka nem született annak a kérdésnek az eldöntésében, hogy valóban található-e a Mecsekben nemesfém-indikáció, illetve nemesfémérc. Amennyiben igen, a további modern szemléletű kutatások az érctípus meghatározására és genetikai modelljének pontosítására fókuszálhatók, illetve együtt a minőségi-mennyiségi paraméterek megadásával az ércesedés gazdasági jelentősége is körvonalazható. A fellelhető írott források kutatásával párhuzamosan tehát megindult a lehetséges ércindikációk felderítése a területen, mely eddig ismeretlen, a forrásokban sem említett nemesfém-ércesedés felfedezéséhez vezetett. Az elvégzett terepi és laboratóriumi vizsgálatok megerősítették, hogy az Ófalu térségében, a Mecsekalja-zónában feltáródó ópaleozoós, milonitosodott metamorf kőzetek (Studervölgyi Gneisz Formáció) olyan Au-Ag- Bi-Te szulfidos-telluridos ércesedést tartalmaznak, mely e kőzetek lepusztulásából származó miocén kavicsanyagban (Szászvári Formáció) is megtalálható. Az érces kavicsokon kívül a durvatörmelékes, folyóvízi eredetű Szászvári Formáció önálló aranyszemcséket is tartalmaz, mely szemcsék valószínű leg torlatos eredetűek. A torlatos arany zárványainak paragenezise szintén egyezést mutat az érces kavicsanyag és az Ófalu mellett kibukkanó metamorf kőzetek érces paragenezisével. A kutatási eredmények alapján tehát a Mecsekalja-zónában egy eddig teljesen ismeretlen, Au-Ag-Bi-Te elemegyüttessel jellemzett orogén aranyércesedés előfordulását azonosítottuk, melynek egy része lepusztult és áthalmozódott a Kelet-Mecsek kora miocén folyóvízi üledékgyűjtőibe.},
	year = {2022},
	eissn = {2559-902X},
	pages = {307-329},
	orcid-numbers = {Jáger, Viktor/0000-0003-1283-5198; Molnár, Ferenc/0000-0002-1873-1915}
}

@{MTMT:3284747,
	title = {A Cassignol-Gillot módszer bevezetése az MTA Atomki IKER Központjában},
	url = {https://m2.mtmt.hu/api/publication/3284747},
	author = {Benkó, Zsolt and Nagy, Dávid and Jáger, Viktor and Szepesi, János and Pécskay, Zoltán and Ott, Ulrich and Kocsisné, Pető Mária},
	booktitle = {Ahol az elemek találkoznak: víz, föld és tűz határán},
	unique-id = {3284747},
	year = {2017},
	pages = {21-24},
	orcid-numbers = {Jáger, Viktor/0000-0003-1283-5198}
}

@{MTMT:3284751,
	title = {Meddig maradhat konszolidálatlan állapotban mélytengeri mésziszap? Peperitképződés a mecseki kora-krétában},
	url = {https://m2.mtmt.hu/api/publication/3284751},
	author = {Jáger, Viktor and Benkó, Zsolt},
	booktitle = {Ahol az elemek találkoznak: víz, föld és tűz határán},
	unique-id = {3284751},
	year = {2017},
	pages = {66-68},
	orcid-numbers = {Jáger, Viktor/0000-0003-1283-5198}
}

@mastersthesis{MTMT:3071375,
	title = {A Kelet-Mecsek kora-kréta vulkanizmusához kapcsolódó hidrotermális folyamatok és ércindikációk},
	url = {https://m2.mtmt.hu/api/publication/3071375},
	author = {Jáger, Viktor},
	doi = {10.15476/ELTE.2015.114},
	publisher = {Eötvös Loránd University},
	unique-id = {3071375},
	year = {2016},
	orcid-numbers = {Jáger, Viktor/0000-0003-1283-5198}
}

@article{MTMT:2814679,
	title = {Csátalja, the largest H4-5 chondrite from Hungary},
	url = {https://m2.mtmt.hu/api/publication/2814679},
	author = {Kovács, János and Sajó, István and Márton, Zsuzsanna and Jáger, Viktor and Hegedüs, Tibor and Berecz, Tibor and Tóth, Tamás Ferenc and Gyenizse, Péter and Podobni, András},
	doi = {10.1016/j.pss.2014.11.009},
	journal-iso = {PLANET SPACE SCI},
	journal = {PLANETARY AND SPACE SCIENCE},
	volume = {105},
	unique-id = {2814679},
	issn = {0032-0633},
	abstract = {We report here for the first time the composition and 
		mineralogical studies on a new meteorite, which was found in 
		August 2012 near the village of Csátalja, Hungary (46°0'21-N; 
		18°59'27'E). The Csátalja meteorite is classified as a H4-5 
		ordinary chondrite with shock stage S2 and a degree of 
		weathering W1 and the total mass is 15 kg. The Csátalja 
		meteorite is characterized by well-defined chondrules composed 
		either of olivine or pyroxene. X-ray diffractogram shows the 
		primary phases olivine, pyroxene, kamacite, and albite. Metal 
		particles were extracted from the bulk powdered samples exhibit 
		only kamacite and small amounts of the intergrowth 
		taenite/kamacite. Raman spectra of forsterite indicate that 
		Csátalja meteorite suffered from relatively low shock pressure 
		regime. The texture of chondrules varies from nonporphyritic 
		(e.g., barred olivine, radial pyroxene) to porphyritic ones 
		(e.g., granular olivine as well as olivine pyroxene). The 
		meteorite name has not yet approved by the Nomenclature 
		Committee of the Meteoritical Society.},
	keywords = {Silicate minerals; olivine; Nanocrystalline materials; Cesium; Hungarians; EBSD; LIBS; Micro-Raman; METEORITES; weathering; ORDINARY CHONDRITES; Csátalja; Ordinary chondrite; Hungarian meteorite},
	year = {2015},
	eissn = {1873-5088},
	pages = {94-100},
	orcid-numbers = {Kovács, János/0000-0001-7742-5515; Sajó, István/0000-0002-1228-1407; Márton, Zsuzsanna/0000-0001-7625-3571; Jáger, Viktor/0000-0003-1283-5198; Berecz, Tibor/0000-0001-9632-8120; Gyenizse, Péter/0000-0002-8175-9734}
}

@article{MTMT:2930627,
	title = {Core-Shell Processing of Natural Pigment: Upper Palaeolithic Red Ochre from Lovas, Hungary},
	url = {https://m2.mtmt.hu/api/publication/2930627},
	author = {Sajó, István and Kovács, János and Fitzsimmons, KE and Jáger, Viktor and Lengyel, György and Viola, B and Talamo, S and Hublin, JJ},
	doi = {10.1371/journal.pone.0131762},
	journal-iso = {PLOS ONE},
	journal = {PLOS ONE},
	volume = {10},
	unique-id = {2930627},
	issn = {1932-6203},
	year = {2015},
	eissn = {1932-6203},
	orcid-numbers = {Sajó, István/0000-0002-1228-1407; Kovács, János/0000-0001-7742-5515; Jáger, Viktor/0000-0003-1283-5198; Lengyel, György/0000-0002-7803-3043}
}

@article{MTMT:2759531,
	title = {Mineralogy of Late Upper Palaeolithic red ochre from Lovas, Hungary},
	url = {https://m2.mtmt.hu/api/publication/2759531},
	author = {Kovács, János and Sajó, István and Jáger, Viktor and Lengyel, György},
	journal-iso = {BUL SHKEN GJEOL},
	journal = {BULETINI I SHKENCAVE GJEOLOGJIKE},
	volume = {50},
	unique-id = {2759531},
	issn = {0254-5276},
	year = {2014},
	eissn = {2306-9600},
	pages = {62-62},
	orcid-numbers = {Kovács, János/0000-0001-7742-5515; Sajó, István/0000-0002-1228-1407; Jáger, Viktor/0000-0003-1283-5198; Lengyel, György/0000-0002-7803-3043}
}

@{MTMT:2752680,
	title = {A mecseki fonolit ritkaföldfém-tartalma és ásványi hordozói},
	url = {https://m2.mtmt.hu/api/publication/2752680},
	author = {Szakáll, Sándor and Jáger, Viktor and Fehér, Béla and Zajzon, Norbert},
	booktitle = {Ritkaföldfémek magyarországi földtani képződményekben},
	unique-id = {2752680},
	year = {2014},
	pages = {47-66},
	orcid-numbers = {Jáger, Viktor/0000-0003-1283-5198}
}

@article{MTMT:2329761,
	title = {An enigmatic source of hematitic carbonate beds containing vast amounts of iron oxidizers in a paleozoic metamorphic complex, South Hungary, Geresd-Hills, Ófalu},
	url = {https://m2.mtmt.hu/api/publication/2329761},
	author = {Jáger, Viktor and Dabi, G and Pekkerné Menyhárt, Adrienn},
	journal-iso = {GEOPHYS RES ABSTR},
	journal = {GEOPHYSICAL RESEARCH ABSTRACTS},
	volume = {15},
	unique-id = {2329761},
	issn = {1029-7006},
	year = {2013},
	eissn = {1607-7962},
	orcid-numbers = {Jáger, Viktor/0000-0003-1283-5198}
}

@{MTMT:2400590,
	title = {Mitől vörös a lovasi okker? – A lovasi okker ásványtani és geokémiai vizsgálata. Lovas ochre, what makes its red color? – Mineralogical and geochemical analyses},
	url = {https://m2.mtmt.hu/api/publication/2400590},
	author = {Kovács, János and Jáger, Viktor and Sajó, I},
	booktitle = {IV. Kőzettani és Geokémiai Vándorgyűlés kiadványa : [Orfű, 2013. szeptember 12-14.]},
	unique-id = {2400590},
	year = {2013},
	pages = {127-128},
	orcid-numbers = {Kovács, János/0000-0001-7742-5515; Jáger, Viktor/0000-0003-1283-5198}
}

@article{MTMT:2421699,
	title = {The connection between iron ore formations and „mud-shrimp” colonizations around sunken wood debris and hydrothermal sediments in a Lower Cretaceous continental rift basin, Mecsek Mts. Hungary.},
	url = {https://m2.mtmt.hu/api/publication/2421699},
	author = {Jáger, Viktor and Molnár, Ferenc and Buchs, D and Kodera, P},
	doi = {10.1016/j.earscirev.2012.06.003},
	journal-iso = {EARTH-SCI REV},
	journal = {EARTH-SCIENCE REVIEWS},
	volume = {114},
	unique-id = {2421699},
	issn = {0012-8252},
	abstract = {In the Early Cretaceous, the continental rift basin of the Mecsek Mts. (Hungary), was situated on the southern edge of the European plate. The opening of the North Atlantic Ocean created a dilatational regime that expanded to the southern edge of the European plate, where several extensional basins and submarine volcanoes were formed during the Early Cretaceous epoch. Permanent seaquake activity caused high swell events during which a large amount of terrestrial wood fragments entered into submarine canyons from rivers or suspended woods which had sunk into the deep seafloor. These fragments created extended wood-fall deposits which contributed large-scale flourishing of numerous burrowing thalassinid crustaceans. Twelve different thalassinid coprolite ichnospecies can be found in the Berriasian-Hauterivian volcanosedimentary formations. According to the seladonitic crustacean burrows which associated with framboidal pyrite containing Zoophycos and Chondrites ichnofossils (i.e. a "fodinichnia" trace fossil association), the bottom water was aerobic and the pore water was anaerobic; in the latter sulfate reduction occurred. The preservation of wood fragments around thalassinid burrows can be explained by rapid sedimentation related to turbidity currents. Due to the low temperature hydrothermal circulations of seawater, large amounts of iron were released from intrusive, pillowed basaltic sills; these sills intruded into soft, water-saturated sediments containing large amounts of thalassinid excrement. In the coprolites can be found idiomorphic mineral particles originating from the basalts, and coprolites can often be found in peperitic interpillow sediments. This indicates that the life-activity of the decapoda crustaceans in many Lower Cretaceous occurrences initially preceded the first magmatic eruptions. The paroxysm of the rift volcanism took place during the Valanginian age, when some submarine volcanoes emerged above sea level, reaching a maximum height of 300 m (above sea level); from these volcanoes further terrestrial plant debris got into the basin. Hydrothermal vents, which periodically occurred around basaltic bodies until the Hauterivian, could have contributed to the creation of favourable temperature or nutritional conditions for some decapoda crustaceans - e.g the recently described new callianassid (Nihonotrypaea thermophila), which is known only from hydrothermally infuenced habitats. Around the intrusive pillow basalts, hydrothermal circulation of oxygenated seawater occured and thick seladonitic and goethitic fills formed along the cracks and cavities of pillowed basalts. When oxidized, sulfaterich fluids passed into the crustacean coprolite-rich, reductive and anaerobic interpillow sediments, these fluids underwent an intensive sulfate reduction. Thiswas primarily due to termophil sulfate reducers which as proved by the negative sulfur isotope values (-35.9‰ and-28.0‰ δ 34S) of sulfidic hydrothermal chimneys which contain framboidal pyrite and which were formed between the pillow basalts. The largest chimney structure reached a height of 1 m, with a mass of about 150 kg. The sulfide phase is characterized by Mo enrichments up to 511 ppm. The fluid inclusion measurements fromthe calcitic precipitations of the sulfide chimneys indicate lowtemperature (~129 °C) hydrothermal activity, and the salinity of the primary fluid inclusions proves the seawater origin of the hydrothermal fluids. In some thalassinid crustacean coprolite rich interpillow sediments and in the cracks of some hydrothermal calcite, there is the presence of black, lustrous bitumine (gilsonite) which is the distillation product of hydrothermal petroleum formed mainly by the coprolites. Hydrothermal circulationsof oxygenated seawater caused subsequent oxidation of the sulfidic, interpillowsediments and chimneys; these were altered to formgoethite. Due to the short-period of the hydrothermal activity among the intrusive pillowed basalts, sulfidized interpillow sediments could not be oxidized completely. The texture of the goethitic iron ore (as an interpillow sediment) is network-like and dentritic, which is very similar to the iron-oxidic and microbial textured sediments of the Juan de Fuca Ridge. The dendritic ironoxide-hydroxide particles which were involved in this study are not hollow and exceed the size-domain characteristic for bacterial products. However, in some cases hollow- and tube-like particles having a diameter of 1.2-1.5 μm can refer to the activity of the Sphaerotilus-Leptothrix iron-oxidizer bacterial group. © 2012 Elsevier B.V.},
	year = {2012},
	eissn = {1872-6828},
	pages = {250-278},
	orcid-numbers = {Jáger, Viktor/0000-0003-1283-5198; Molnár, Ferenc/0000-0002-1873-1915}
}

@article{MTMT:2156898,
	title = {Földtani érvek, melyek a zengővárkonyi alsó-kréta "hidrotermás-fauna" ellen szólnak = Geological arguments which militate against the Lower Cretaceous Zengo{double acute}várkony "hydrothermal fauna". Kritikai hozzászólás Bujtor L. "A mecseki alsó-kréta (valangini) hidrotermális hasadékkitöltés őslénytani jellege" című dolgozatához (Földtani Közlöny 142/2, 137-148.))},
	url = {https://m2.mtmt.hu/api/publication/2156898},
	author = {Jáger, Viktor},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {142},
	unique-id = {2156898},
	issn = {0015-542X},
	year = {2012},
	eissn = {2559-902X},
	pages = {379-384},
	orcid-numbers = {Jáger, Viktor/0000-0003-1283-5198}
}

@article{MTMT:1709663,
	title = {Tenger alatti hévforrások és ércesedések a Mecsekben},
	url = {https://m2.mtmt.hu/api/publication/1709663},
	author = {Jáger, Viktor},
	journal-iso = {TERMÉSZET VILÁGA},
	journal = {TERMÉSZET VILÁGA},
	volume = {142},
	unique-id = {1709663},
	issn = {0040-3717},
	year = {2011},
	pages = {6-9},
	orcid-numbers = {Jáger, Viktor/0000-0003-1283-5198}
}

@article{MTMT:1384578,
	title = {Volcanic architecture, eruption mechanism and landform evolution of a Plio/Pleistocene intracontinental basaltic polycyclic monogenetic volcano from the Bakony-Balaton Highland Volcanic Field, Hungary},
	url = {https://m2.mtmt.hu/api/publication/1384578},
	author = {Kereszturi, G and Csillag, Gábor and Németh, Károly and Sebe, Krisztina and Balogh, Kadosa and Jáger, Viktor},
	doi = {10.2478/v10085-010-0019-2},
	journal-iso = {CENT EUR J GEOSCI},
	journal = {CENTRAL EUROPEAN JOURNAL OF GEOSCIENCES},
	volume = {2},
	unique-id = {1384578},
	issn = {2081-9900},
	abstract = {Bondoró Volcanic Complex (shortly Bondoró) is one of the most complex eruption centre of Bakony-Balaton Highland Volcanic Field, which made up from basaltic pyroclastics sequences, a capping confined lava field (~4 km 2) and an additional scoria cone. Here we document and describe the main evolutional phases of the Bondoró on the basis of facies analysis, drill core descriptions and geomorphic studies and provide a general model for this complex monogenetic volcano. Based on the distinguished 13 individual volcanic facies, we infer that the eruption history of Bondoró contained several stages including initial phreatomagmatic eruptions, Strombolian-type scoria cones forming as well as effusive phases. The existing and newly obtained K-Ar radiometric data have confirmed that the entire formation of the Bondoró volcano finished at about 2.3 Ma ago, and the time of its onset cannot be older than 3.8 Ma. Still K-Ar ages on neighbouring formations (e.g. Kab-hegy, Agár-teto) do not exclude a long-lasting eruptive period with multiple eruptions and potential rejuvenation of volcanic activity in the same place indicating stable melt production beneath this location. The prolonged volcanic activity and the complex volcanic facies architecture of Bondoró suggest that this volcano is a polycyclic volcano, composed of at least two monogenetic volcanoes formed more or less in the same place, each erupted through distinct, but short lived eruption episodes. The total estimated eruption volume, the volcanic facies characteristics and geomorphology also suggests that Bondoró is rather a small-volume polycyclic basaltic volcano than a polygenetic one and can be interpreted as a nested monogenetic volcanic complex with multiple eruption episodes. It seems that Bondoró is rather a "rule" than an "exception" in regard of its polycyclic nature not only among the volcanoes of the Bakony-Balaton Highland Volcanic Field but also in the Neogene basaltic volcanoes of the Pannonian Basin.},
	keywords = {SCORIA CONE; MAAR; polygenetic; polycyclic; monogenetic},
	year = {2010},
	eissn = {1896-1517},
	pages = {362-384},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199; Jáger, Viktor/0000-0003-1283-5198}
}

@CONFERENCE{MTMT:2851254,
	title = {Lower Cretaceous continental rift-type black smoker system in the East Mecsek Mts},
	url = {https://m2.mtmt.hu/api/publication/2851254},
	author = {Jáger, Viktor and Molnár, Ferenc},
	booktitle = {Mitteilungen der Österreichischen Mineralogischen Gesellschaft},
	unique-id = {2851254},
	year = {2008},
	pages = {70},
	orcid-numbers = {Jáger, Viktor/0000-0003-1283-5198; Molnár, Ferenc/0000-0002-1873-1915}
}

@article{MTMT:2329774,
	title = {Metasomatic-hydrothermal processes along the contact zone of Lower Cretaceous magmatic sills intruded into Lower Jurassic coal beds at Pécs-Vasas, Mecsek Mts., Hungary},
	url = {https://m2.mtmt.hu/api/publication/2329774},
	author = {Jáger, Viktor and Molnár, Ferenc},
	journal-iso = {ACTA MINERAL PETROGR ABSTRACT SER},
	journal = {ACTA MINERALOGICA PETROGRAPHICA - ABSTRACT SERIES},
	volume = {5},
	unique-id = {2329774},
	issn = {1589-4835},
	year = {2006},
	pages = {50},
	orcid-numbers = {Jáger, Viktor/0000-0003-1283-5198; Molnár, Ferenc/0000-0002-1873-1915}
}

@book{MTMT:1532289,
	title = {Az ásványok világa. a Herman Ottó Múzeum utazó kiállítása általános és középiskolák számára},
	url = {https://m2.mtmt.hu/api/publication/1532289},
	isbn = {9639271519},
	author = {Szakáll, Sándor and Fehér, Béla and Jáger, Viktor},
	publisher = {HOM; Miskolci Herman Ottó Múzeum},
	unique-id = {1532289},
	year = {2006},
	orcid-numbers = {Jáger, Viktor/0000-0003-1283-5198}
}

@CONFERENCE{MTMT:2151064,
	title = {Metasomatic-hydrothermal processes along the contact zone of a tephritic sill and black shale in the Eastern Mecsek Mts., South-Hungary},
	url = {https://m2.mtmt.hu/api/publication/2151064},
	author = {Jáger, Viktor and Molnár, Ferenc},
	booktitle = {Acta Mineralogica-Petrographica, Abstract Series 1},
	unique-id = {2151064},
	year = {2003},
	orcid-numbers = {Jáger, Viktor/0000-0003-1283-5198; Molnár, Ferenc/0000-0002-1873-1915}
}

@article{MTMT:1709632,
	title = {Ritkaságok a Keleti-Mecsek ásványvilágából},
	url = {https://m2.mtmt.hu/api/publication/1709632},
	author = {Jáger, Viktor},
	journal-iso = {FÖLDTANI KUTATÁS},
	journal = {FÖLDTANI KUTATÁS},
	volume = {35},
	unique-id = {1709632},
	issn = {0133-2422},
	year = {1998},
	pages = {19-22},
	orcid-numbers = {Jáger, Viktor/0000-0003-1283-5198}
}