@article{MTMT:31811016,
	title = {Rapid determination of full and empty adeno-associated virus capsid ratio by capillary isoelectric focusing},
	url = {https://m2.mtmt.hu/api/publication/31811016},
	author = {Li, Tingting and Gao, Tie and Chen, Hongxu and Pekker, Péter and Pekkerné Menyhárt, Adrienn and Guttman, András},
	doi = {10.2174/1566524020666200915105456},
	journal-iso = {CURR MOL MED},
	journal = {CURRENT MOLECULAR MEDICINE},
	volume = {20},
	unique-id = {31811016},
	issn = {1566-5240},
	year = {2020},
	eissn = {1875-5666},
	pages = {814-820},
	orcid-numbers = {Pekker, Péter/0000-0002-0463-0742; Guttman, András/0000-0002-7838-082X}
}

@article{MTMT:3005440,
	title = {Richelsdorfite Ca2Cu5Sb(AsO4)4(OH)6Cl 6H2O and turquoise Cu(Al,Fe)6(PO4)4(OH)8 5H2O from Parádfürdő ore deposite, Fehérkő Hill, Hungary},
	url = {https://m2.mtmt.hu/api/publication/3005440},
	author = {Pekkerné Menyhárt, Adrienn and Szakáll, Sándor},
	journal-iso = {ACTA MINERAL PETROGR ABSTRACT SER},
	journal = {ACTA MINERALOGICA PETROGRAPHICA - ABSTRACT SERIES},
	volume = {9},
	unique-id = {3005440},
	issn = {1589-4835},
	year = {2015},
	pages = {41-41}
}

@article{MTMT:2563071,
	title = {Arzenátok a Velencei-hegységi Likas-kőről},
	url = {https://m2.mtmt.hu/api/publication/2563071},
	author = {Pekkerné Menyhárt, Adrienn and Szakáll, Sándor},
	journal-iso = {GEODA},
	journal = {GEODA},
	volume = {32},
	unique-id = {2563071},
	issn = {2060-212X},
	year = {2013},
	pages = {3-16}
}

@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}
}

@article{MTMT:1953865,
	title = {Beudantite [PbFe3+3(AsO4)(SO4)(OH)6] - Segnitite [PbFe3+3(AsO4)2(OH)6] solid solution from Likas-kő, Velence Hills, Hungary},
	url = {https://m2.mtmt.hu/api/publication/1953865},
	author = {Pekkerné Menyhárt, Adrienn and Zajzon, Norbert and Szakáll, Sándor},
	journal-iso = {ACTA MINERAL PETROGR ABSTRACT SER},
	journal = {ACTA MINERALOGICA PETROGRAPHICA - ABSTRACT SERIES},
	volume = {7},
	unique-id = {1953865},
	issn = {1589-4835},
	year = {2012},
	pages = {88-88}
}

@article{MTMT:2162209,
	title = {New mineralogical data concerning volcanites from the district of Mád, in North East Hungary (Tokaj Mts)},
	url = {https://m2.mtmt.hu/api/publication/2162209},
	author = {Pekkerné Menyhárt, Adrienn and Dódony, István and Pekker, Péter},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {141},
	unique-id = {2162209},
	issn = {0015-542X},
	abstract = {This study presents new data on mordenite and clinoptilolite, rectorite, iron oxide, halloysite, smectite and SiO 2 phases from quarries in hydrothermally altered rhyolite tuff, in the environs of Mád, Tokaj Mts., NE Hungary. X-ray powder diffraction (XRPD), scanning (SEM) and transmission electron microscopic (TEM, HRTEM, ATEM) techniques were used to identify minerals and gain more details about their occurrence. An unusual iron oxide/hydroxide phase (that had earlier been considered as haematite/hydrohaematite) was recognised at Király Hill. Although its XRPD diagram shows reflections which can be interpreted as haematite, according to TEM data neither its structure nor its chemical composition comply with that of haematite. Király Hill was identified as a new locality of halloysite. The X-ray powder diffraction study of a sample from the Bomboly area indicates rectorite (as was known earlier); however, TEM images show only separate illite and smectite crystals, without any evident structural interrelation between them. A Suba-oldal smectite and an SiO 2 phase can also be found. Using TEM the thickness of the individual smectite flakes was determined and the SiO 2 phase could be identified as cristobalite (HRTEM- high resolution TEM). The zeolite minerals were identified on the basis of sets of their D (hkl) values and symmetries measured on selected areaelectron diffraction patterns (SAED). Their respective compositions were quantified simultaneously using energy dispersive X-ray (EDX) spectra which were acquired on the corresponding areas. The hydrothermally altered rhyolite tuff at Harcsa-teto{double acute} (Harcsa Hill) contains an Na-free, Ca-containing zeolite; according to XRPD results this corresponds to mordenite. On the other hand, in the Suba-oldal area clinoptilolite occurs with additional Mg and K as exchangeable cations.},
	keywords = {clinoptilolite; CRISTOBALITE; Halloysite; smectite; Tokaj Mts; MORDENITE; Rectorite; Iron-oxide},
	year = {2011},
	eissn = {2559-902X},
	pages = {257-266},
	orcid-numbers = {Pekker, Péter/0000-0002-0463-0742}
}

@article{MTMT:1985048,
	title = {Gartrellite and other arsenates from Likaskő, Velence Hills (Hungary)},
	url = {https://m2.mtmt.hu/api/publication/1985048},
	author = {Pekkerné Menyhárt, Adrienn and Szakáll, Sándor},
	journal-iso = {ACTA MINERAL PETROGR ABSTRACT SER},
	journal = {ACTA MINERALOGICA PETROGRAPHICA - ABSTRACT SERIES},
	volume = {6},
	unique-id = {1985048},
	issn = {1589-4835},
	year = {2010},
	pages = {434-434}
}