@article{MTMT:32467230,
	title = {Synthetic fluid inclusions XXIV. In situ monitoring of the carbonation of olivine under conditions relevant to carbon capture and storage using synthetic fluid inclusion micro-reactors: Determination of reaction rates},
	url = {https://m2.mtmt.hu/api/publication/32467230},
	author = {Sendula, Eszter and Héctor, M. Lamadrid and J., Donald Rimstidt and Matthew, Steele-MacInnis and D., Matthew Sublett Jr. and Aradi, László Előd and Szabó, Csaba and Mark, J. Caddick and Zoltán, Zajacz and Robert, J. Bodnar},
	doi = {10.3389/fclim.2021.722447},
	journal-iso = {FRONT CLIM},
	journal = {FRONTIERS IN CLIMATE},
	volume = {3},
	unique-id = {32467230},
	year = {2021},
	eissn = {2624-9553},
	orcid-numbers = {Aradi, László Előd/0000-0003-0276-3119; Szabó, Csaba/0000-0002-1580-6344}
}

@article{MTMT:31844027,
	title = {Raman spectral behavior of N2, CO2, and CH4 in N2-CO2-CH4 gas mixtures from 22 °C to 200 °C and 10 to 500 bars, with application to other gas mixtures},
	url = {https://m2.mtmt.hu/api/publication/31844027},
	author = {Sublett, Jr D. Matthew and Sendula, Eszter and Lamadrid, Hector M. and Steele-MacInnis, Matthew and Spiekermann, Georg and Bodnar, Robert J.},
	doi = {10.1002/jrs.6033},
	journal-iso = {J RAMAN SPECTROSC},
	journal = {JOURNAL OF RAMAN SPECTROSCOPY},
	volume = {52},
	unique-id = {31844027},
	issn = {0377-0486},
	year = {2021},
	eissn = {1097-4555},
	pages = {750-769}
}

@article{MTMT:31844028,
	title = {Combined LA-ICP-MS and cryo-SEM-EDS: An improved technique for quantitative analysis of major, minor, and trace elements in fluid inclusions in halite},
	url = {https://m2.mtmt.hu/api/publication/31844028},
	author = {Weldeghebriel, Mebrahtu F. and Lowenstein, Tim K. and Garcia-Veigas, Javier and Collins, David and Sendula, Eszter and Bodnar, Robert J. and Graney, Joseph R. and Cendon, Dioni I and Lensky, Nadav G. and Mor, Ziv and Sirota, Ido},
	doi = {10.1016/j.chemgeo.2020.119762},
	journal-iso = {CHEM GEOL},
	journal = {CHEMICAL GEOLOGY},
	volume = {551},
	unique-id = {31844028},
	issn = {0009-2541},
	year = {2020},
	eissn = {1872-6836},
	orcid-numbers = {Weldeghebriel, Mebrahtu F./0000-0002-0095-6235; Garcia-Veigas, Javier/0000-0003-2225-2682}
}

@article{MTMT:31578323,
	title = {Shift in the Raman symmetric stretching band of N-2, CO2, and CH4 as a function of temperature, pressure, and density},
	url = {https://m2.mtmt.hu/api/publication/31578323},
	author = {Sublett, D. Matthew Jr. and Sendula, Eszter and Lamadrid, Hector and Steele-MacInnis, Matthew and Spiekermann, Georg and Burruss, Robert C. and Bodnar, Robert J.},
	doi = {10.1002/jrs.5805},
	journal-iso = {J RAMAN SPECTROSC},
	journal = {JOURNAL OF RAMAN SPECTROSCOPY},
	volume = {51},
	unique-id = {31578323},
	issn = {0377-0486},
	abstract = {The Raman spectra of pure N-2, CO2, and CH4 were analyzed over the range 10 to 500 bars and from -160 degrees C to 200 degrees C (N-2), 22 degrees C to 350 degrees C (CO2), and -100 degrees C to 450 degrees C (CH4). At constant temperature, Raman peak position, including the more intense CO2 peak (nu+), decreases (shifts to lower wave number) with increasing pressure for all three gases over the entire pressure and temperature (PT) range studied. At constant pressure, the peak position for CO2 and CH4 increases (shifts to higher wave number) with increasing temperature over the entire PT range studied. In contrast, N-2 first shows an increase in peak position with increasing temperature at constant pressure, followed by a decrease in peak position with increasing temperature. The inflection temperature at which the trend reverses for N-2 is located between 0 degrees C and 50 degrees C at pressures above similar to 50 bars and is pressure dependent. Below similar to 50 bars, the inflection temperature was observed as low as -120 degrees C. The shifts in Raman peak positions with PT are related to relative density changes, which reflect changes in intermolecular attraction and repulsion. A conceptual model relating the Raman spectral properties of N-2, CO2, and CH4 to relative density (volume) changes and attractive and repulsive forces is presented here. Additionally, reduced temperature-dependent densimeters and barometers are presented for each pure component over the respective PT ranges. The Raman spectral behavior of the pure gases as a function of temperature and pressure is assessed to provide a framework for understanding the behavior of each component in multicomponent N-2-CO2-CH4 gas systems in a future study.},
	keywords = {FLUIDS; ATTRACTION; REPULSION; wave number},
	year = {2020},
	eissn = {1097-4555},
	pages = {555-568}
}

@article{MTMT:31044367,
	title = {Metasomatism-induced wehrlite formation in the upper mantle beneath the Nógrád-Gömör Volcanic Field (Northern Pannonian Basin): Evidence from xenoliths},
	url = {https://m2.mtmt.hu/api/publication/31044367},
	author = {Patkó, Levente and Liptai, Nóra and Aradi, László Előd and Klébesz, Rita and Sendula, Eszter and Bodnar, Robert J. and Kovács, István János and Hidas, Károly and Cesare, Bernardo and Novák, Attila and Trásy, Balázs and Szabó, Csaba},
	doi = {10.1016/j.gsf.2019.09.012},
	journal-iso = {GEOSCI FRONT},
	journal = {GEOSCIENCE FRONTIERS},
	volume = {11},
	unique-id = {31044367},
	issn = {1674-9871},
	year = {2020},
	eissn = {1674-9871},
	pages = {943-964},
	orcid-numbers = {Patkó, Levente/0000-0001-6007-3103; Liptai, Nóra/0000-0002-2464-2468; Aradi, László Előd/0000-0003-0276-3119; Kovács, István János/0000-0002-3488-3716; Szabó, Csaba/0000-0002-1580-6344}
}

@article{MTMT:30856441,
	title = {The characteristics of wehrlite forming mantle metasomatism - a silicate melt inclusion study in upper mantle xenoliths from Mediterranean Region},
	url = {https://m2.mtmt.hu/api/publication/30856441},
	author = {Patkó, Levente and Hidas, Károly and Sendula, Eszter and Liptai, Nóra and Aradi, László Előd and Berkesi, Márta and Robert, J. Bodnar and Carlos, J. Garrido and Szabó, Csaba},
	journal-iso = {ACTA MINERAL PETROGR ABSTRACT SER},
	journal = {ACTA MINERALOGICA PETROGRAPHICA - ABSTRACT SERIES},
	volume = {10},
	unique-id = {30856441},
	issn = {1589-4835},
	year = {2019},
	pages = {98},
	orcid-numbers = {Patkó, Levente/0000-0001-6007-3103; Liptai, Nóra/0000-0002-2464-2468; Aradi, László Előd/0000-0003-0276-3119; Berkesi, Márta/0000-0003-4380-057X; Szabó, Csaba/0000-0002-1580-6344}
}

@{MTMT:31286124,
	title = {The relevance of dawsonite precipitation in CO2 sequestration in the Mihályi–Répcelak area, NW Hungary.},
	url = {https://m2.mtmt.hu/api/publication/31286124},
	author = {KIRÁLY, CS and Sendula, Eszter and Szamosfalvi, Ágnes and KÁLDOS, R. and Kónya, Péter and Kovács, István János and Füri, Judit Izabella and BENDŐ, ZS. and Falus, György},
	booktitle = {Reservoir quality of clastic and carbonate rocks: analysis, modelling and prediction},
	unique-id = {31286124},
	abstract = {A natural CO2 reservoir system with a sandstone lithology in NW Hungary has been studied due to its similarities to a large saline reservoir formation that is widespread in the the Pannonian Basin (Central Europe) and is suggested to be one of the best candidates for industrial CO2 storage. A range of analytical techniques has been used on core samples from CO2-containing sandstone layers that represent a wide range of pressures (90–155 bar), temperatures (79–958C) and pore fluid compositions (total dissolved solids between 18 000 and 50 700 mg l21) to identify the mineralogy and textural characteristics of the natural reservoir. The only clear CO2-related feature in the studied lithology was the occurrence of dawsonite (NaAlCO3(OH)2) in a close textural relationship with albite. This is in clear agreement with our geochemical modelling results, which also underline the presence of albite as a precondition for the crystallization of dawsonite at the given P–T–X conditions. Our results suggest that, at least in the Pannonian Basin, dawsonite may be an important mineral for the safe sequestration of industrial CO2 in the subsurface.},
	keywords = {CO2; Dawsonite; Mihályi-Répcelak; NW Hungary},
	year = {2018},
	pages = {405-405},
	orcid-numbers = {Kovács, István János/0000-0002-3488-3716}
}

@article{MTMT:3362505,
	title = {Deciphering mantle metasomatism using silicate melt inclusions beneath the Nógrád-Gömör Volcanic Field (Northern Pannonian Basin)},
	url = {https://m2.mtmt.hu/api/publication/3362505},
	author = {Patkó, Levente and Liptai, Nóra and Aradi, László Előd and Robert, Bodnar and Sendula, Eszter and Kovács, István János and Klébesz, Rita and Szabó, Csaba},
	journal-iso = {GEOPHYS RES ABSTR},
	journal = {GEOPHYSICAL RESEARCH ABSTRACTS},
	volume = {20},
	unique-id = {3362505},
	issn = {1029-7006},
	year = {2018},
	eissn = {1607-7962},
	orcid-numbers = {Patkó, Levente/0000-0001-6007-3103; Liptai, Nóra/0000-0002-2464-2468; Aradi, László Előd/0000-0003-0276-3119; Kovács, István János/0000-0002-3488-3716; Szabó, Csaba/0000-0002-1580-6344}
}

@article{MTMT:3082983,
	title = {The relevance of dawsonite precipitation in CO2 sequestration in the Mihályi-Répcelak area, NW Hungary},
	url = {https://m2.mtmt.hu/api/publication/3082983},
	author = {Király, Csilla and Sendula, Eszter and Szamosfalvi, Ágnes and Káldos, Réka and Kónya, Péter and Kovács, István János and Füri, Judit Izabella and Zsolt, Bendő and Falus, György},
	doi = {10.1144/SP435.15},
	journal-iso = {GEOL SOC SPEC PUBL},
	journal = {GEOLOGICAL SOCIETY SPECIAL PUBLICATIONS},
	volume = {435},
	unique-id = {3082983},
	issn = {0305-8719},
	keywords = {CO2; Dawsonite; Mihályi-Répcelak; NW Hungary},
	year = {2018},
	eissn = {2041-4927},
	pages = {405-418},
	orcid-numbers = {Kovács, István János/0000-0002-3488-3716}
}

@article{MTMT:31844031,
	title = {Detailed mineralogical and petrographic analysis of the caprock from a natural CO2 occurrence in Hungary},
	url = {https://m2.mtmt.hu/api/publication/31844031},
	author = {Király, Csilla and Szamosfalvi, Agnes and Zilahi-Sebess, Laszlo and Sendula, Eszter and Kovacs, Istvan and Kónya, Péter and Udvardi, Beatrix and Szabo, Zsuzsanna and Szabó, Csaba and Falus, Gyorgy},
	doi = {10.1016/j.egypro.2017.03.1634},
	journal-iso = {ENERGY PROCEDIA},
	journal = {ENERGY PROCEDIA},
	volume = {114},
	unique-id = {31844031},
	year = {2017},
	eissn = {1876-6102},
	pages = {4926-4933},
	orcid-numbers = {Szabó, Csaba/0000-0002-1580-6344}
}