@CONFERENCE{MTMT:3429216,
	title = {Correlation of basement units from the Pannonian basin and surrounding areas based on lithological associations and the distribution of tectonometamorphic imprints (keynote talk)},
	url = {https://m2.mtmt.hu/api/publication/3429216},
	author = {Schuster, R and Reiser, M and Linner, M and Dégi, Júlia and Király, Edit and Mandl, GW},
	booktitle = {15th Meeting of the Central European Tectonic Studies Group (CETeG)},
	unique-id = {3429216},
	year = {2017},
	pages = {18-19}
}

@CONFERENCE{MTMT:3429215,
	title = {Evolution history of a single garnet (Kő-hegy, Sopron Mountains, Hungary) based on major- and trace-element studies by EPMA, micro-PIXE and LA-ICP-MS},
	url = {https://m2.mtmt.hu/api/publication/3429215},
	author = {Király, Edit and Török, Kálmán and Dégi, Júlia and Kertész, Zs and Abart, R},
	booktitle = {15th Meeting of the Central European Tectonic Studies Group (CETeG)},
	unique-id = {3429215},
	year = {2017},
	pages = {35-36}
}

@{MTMT:3429206,
	title = {A Soproni Gneisz csillámainak nyomelem-geokémiai változásai a magmás–metamorf fejlődéstörténet tükrében},
	url = {https://m2.mtmt.hu/api/publication/3429206},
	author = {Török, Kálmán and Király, Edit and Dégi, Júlia},
	booktitle = {Ahol az elemek találkoznak: víz, föld és tűz határán},
	unique-id = {3429206},
	year = {2017},
	pages = {164-167}
}

@book{MTMT:3257498,
	title = {Ahol az elemek találkoznak: víz, föld és tűz határán. 8. Kőzettani és Geokémiai Vándorgyűlés},
	url = {https://m2.mtmt.hu/api/publication/3257498},
	isbn = {9789636713119},
	editor = {Dégi, Júlia and Király, Edit and Kónya, Péter and Kovács, István János and Pál-Molnár, Elemér and Thamóné Bozsó, Edit and Török, Kálmán and Udvardi, Beatrix},
	publisher = {Magyar Földtani és Geofizikai Intézet},
	unique-id = {3257498},
	year = {2017},
	orcid-numbers = {Kovács, István János/0000-0002-3488-3716; Pál-Molnár, Elemér/0000-0002-9606-0133}
}

@CONFERENCE{MTMT:3429220,
	title = {Submicron scale 3D investigation of kelyphyites after garnet: thermodynamics, crystallographic orientation, microstructure evolution and fluid-rock interactions},
	url = {https://m2.mtmt.hu/api/publication/3429220},
	author = {Dégi, Júlia and Török, Kálmán and Németh, Bianka and Rhede, D and Takács, Ágnes and Habler, G and Abart, R},
	booktitle = {European Geosciences Union (EGU) General Assembly 2016: Conference Abstracts},
	unique-id = {3429220},
	year = {2016},
	pages = {1062},
	orcid-numbers = {Németh, Bianka/0000-0001-9079-9773}
}

@inproceedings{MTMT:3429208,
	title = {A kő-hegyi (Soproni-hegység) gránátok magmás és metamorf képződésének körülményei EMPA, PIXE és LA-ICP-MS vizsgálatok alapján},
	url = {https://m2.mtmt.hu/api/publication/3429208},
	author = {Király, Edit and Török, Kálmán and Dégi, Júlia and Kertész, Zs and Abart, R},
	booktitle = {Itt az idő! : kőzettani-geokémiai folyamatok és azok geokronológiai vonatkozásai},
	unique-id = {3429208},
	year = {2016},
	pages = {45-48}
}

@CONFERENCE{MTMT:3178634,
	title = {Tertiary geodynamics of the Carpathian-Pannonian region and the evolution of its subcontinental lithospheric mantle},
	url = {https://m2.mtmt.hu/api/publication/3178634},
	author = {Kovács, István János and Falus, György and Szabó, Csaba and Török, Kálmán and Hidas, K and Berkesi, Márta and Pintér, Zs and Dégi, Júlia and Liptai, Nóra and Patkó, Levente and Aradi, László Előd and Németh, Bianka and Kiss, János and Fancsik, Tamás},
	booktitle = {XVIII. Nemzetközi Bányászati, Kohászati és Földtani Konferencia},
	unique-id = {3178634},
	keywords = {Carpathian-Pannonian region; geodynamics; földtan},
	year = {2016},
	pages = {16-17},
	orcid-numbers = {Kovács, István János/0000-0002-3488-3716; Szabó, Csaba/0000-0002-1580-6344; Berkesi, Márta/0000-0003-4380-057X; Liptai, Nóra/0000-0002-2464-2468; Patkó, Levente/0000-0001-6007-3103; Aradi, László Előd/0000-0003-0276-3119; Németh, Bianka/0000-0001-9079-9773; Kiss, János/0000-0001-8589-1364}
}

@CONFERENCE{MTMT:3014225,
	title = {Very Dry Lower Crust beneath the Central Part of the Carpathian-Pannonian Region: The Role of Miocene Extension Induced Melting.},
	url = {https://m2.mtmt.hu/api/publication/3014225},
	author = {Kovács, István János and Németh, Bianka and Török, Kálmán and Dégi, Júlia and Fancsik, Tamás},
	booktitle = {25th V.M. Goldschmidt Conference},
	unique-id = {3014225},
	abstract = {The internal part of the CPR is a young extensional basin,
		 which was formed during the Miocene. The central part of the
		 area went through considerable thinning during this extension,
		 when the crust was thinned from its original 50-60 km
		 thickness to the present 25-30 km. The lower crust was
		 sampled by alkaline basaltic volcanoes after the Miocene
		 extension.
		 The granulite xenoliths entrained in these basalts may bear
		 imprints of this preceding extension event. The studied lower
		 crustal xenoliths are metapelites and metabasic rocks having
		 most commonly granoblastic texture. The rock-forming
		 minerals (garnet, pyroxenes, feldspar, sillimanite, rutile) were
		 measured by micro-FTIR spectrometry to determine their
		 ‘water’ content and its substitution mechanism. The NAMs in
		 granulites have usually very low ‘water’ content with bulk
		 water contents typically below 100 ppm. In particular garnet is
		 absolutely dry in all but four xenoliths. Feldspar and
		 orthopyroxene show water contents typically below 100 ppm.
		 The most ‘water’ rich minerals are clinopyroxene and
		 sillimanite containing usually more than 100 ppm water.
		 These concentrations are generally much lower than those
		 have been reported for other lower crustal granulites from
		 China [1] [2]. The very low ‘water’ content of NAMs in lower
		 crustal granulite xenoliths from the central part of the CPR
		 may be the consequence of the Miocene thinning. The
		 accompanying localized fluid infiltration and potential increase
		 in temperature may have resulted in heterogeneous melting and
		 melt extraction from the lower crust having left behind a
		 generally very dry residue. In summary the studied granulite
		 xenoliths highlight that the lower crust in young extensional
		 settings may be generally much depleted in ‘water’.},
	keywords = {petrology; geodynamics; környezetgeokémia; földtan},
	year = {2015},
	pages = {1675-1675},
	orcid-numbers = {Kovács, István János/0000-0002-3488-3716; Németh, Bianka/0000-0001-9079-9773}
}

@article{MTMT:3004642,
	title = {Orthopyroxene-enrichment in the Iherzolite-websterite xenolith suite from Paleogene alkali basalts of the Poiana Rusca Mountains (Romania)},
	url = {https://m2.mtmt.hu/api/publication/3004642},
	author = {Nédli, Zsuzsanna and Szabó, Csaba and Dégi, Júlia},
	doi = {10.1515/geoca-2015-0041},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {66},
	unique-id = {3004642},
	issn = {1335-0552},
	abstract = {In this paper we present the petrography and geochemistry of a recently collected lherzolite-websterite xenolith series and of clinopyroxene xenocrysts, hosted in Upper Cretaceous-Paleogene basanites of Poiana Rusca (Romania), whose xenoliths show notable orthopyroxene-enrichment. In the series a slightly deformed porphyroclastic-equigranular textured series could represent the early mantle characteristics, and in many cases notable orthopyroxene growth and poikilitic texture formation was observed. The most abundant mantle lithology, Type A xenoliths have high Al- and Na-contents but low mg# of the pyroxenes and low cr# of spinel suggesting a low degree (< 10 %) of mafic melt removal. They are also generally poor in overall REE-s (rare earth elements) and have flat REY (rare earth elements + Y) patterns with slight LREE-depletion. The geochemistry of the Type A xenoliths and calculated melt composition in equilibrium with the xenolith clinopyroxenes suggests that the percolating melt causing the poikilitization can be linked to a mafic, Al-Na-rich, volatile-poor melt and show similarity with the Late Cretaceous-Paleogene (66-72 Ma) subduction-related andesitic magmatism of Poiana Rusca. Type B xenoliths, with their slightly different chemistry, suggest that, after the ancient depletion, the mantle went through a slight metasomatic event. A subsequent passage of mafic melts in the mantle, with similar compositions to the older andesitic magmatism of Poiana Rusca, is recorded in the pyroxenites (Fe-rich xenoliths), whereas the megacrysts seem to be cogenetic with the host basanite. The Poiana Rusca xenoliths differ from the orthopyroxene-enriched mantle xenoliths described previously from the Carpathian-Pannonian Region and from the Dacia block.},
	keywords = {TRACE-ELEMENTS; CANARY-ISLANDS; Alkali basalt; Geochemistry; Paleogene; Peridotite xenoliths; Central-Europe; CENTRAL PANNONIAN BASIN; South Carpathians; METASOMATIC AGENT; SILICA ENRICHMENT; EAST SERBIA; LITHOSPHERIC MANTLE BENEATH; mantle xenolith petrology; S Carpathians},
	year = {2015},
	eissn = {1336-8052},
	pages = {499-514},
	orcid-numbers = {Szabó, Csaba/0000-0002-1580-6344}
}

@{MTMT:2943619,
	title = {Distinction of Variscan, Permo-Triassic and Alpine events in andalusite-biotite-sillimanite schists from Sopron area, W-Hungary},
	url = {https://m2.mtmt.hu/api/publication/2943619},
	author = {Dégi, Júlia and Török, Kálmán and Schuster, R},
	booktitle = {CETEG 2015},
	unique-id = {2943619},
	year = {2015},
	pages = {12-12}
}