@article{MTMT:31850039,
	title = {Evolution of deformation mechanism and fluid flow in two pre-rift siliciclastic deposits (Pannonian Basin, Hungary)},
	url = {https://m2.mtmt.hu/api/publication/31850039},
	author = {Beke, Barbara and Laczkó-Dobos, Emese and Hips, Kinga and Schubert, Félix and Petrik, Attila and Milovský, R and Fodor, László},
	doi = {10.1016/j.gloplacha.2021.103434},
	journal-iso = {GLOBAL PLANET CHANGE},
	journal = {GLOBAL AND PLANETARY CHANGE},
	volume = {199},
	unique-id = {31850039},
	issn = {0921-8181},
	year = {2021},
	eissn = {1872-6364},
	orcid-numbers = {Beke, Barbara/0000-0003-0797-1195; Hips, Kinga/0000-0003-2315-120X; Schubert, Félix/0000-0001-8647-5354}
}

@mastersthesis{MTMT:32055542,
	title = {Diagenesis and reservoir quality of Pannonian lacustrine deposits in the Makó Trough, SE Hungary},
	url = {https://m2.mtmt.hu/api/publication/32055542},
	author = {Laczkó-Dobos, Emese},
	doi = {10.15476/ELTE.2019.159},
	publisher = {Eötvös Loránd University},
	unique-id = {32055542},
	year = {2020}
}

@{MTMT:31936889,
	title = {Szerkezeti elemek és a diagenezis kapcsolata porózus, sziliciklasztos üledékekben ÉK-magyarországon.},
	url = {https://m2.mtmt.hu/api/publication/31936889},
	author = {Beke, Barbara and Laczkó-Dobos, Emese and Hips, Kinga and Schubert, Félix and Petrik, Attila and Fodor, László},
	booktitle = {Átalakulások},
	unique-id = {31936889},
	year = {2020},
	pages = {19-21},
	orcid-numbers = {Beke, Barbara/0000-0003-0797-1195; Hips, Kinga/0000-0003-2315-120X; Schubert, Félix/0000-0001-8647-5354}
}

@article{MTMT:31783545,
	title = {Porosity Development Controlled by Deep-Burial Diagenetic Process in Lacustrine Sandstones Deposited in a Back-Arc Basin (Makó Trough, Pannonian Basin, Hungary)},
	url = {https://m2.mtmt.hu/api/publication/31783545},
	author = {Laczkó-Dobos, Emese and Gier, S and Sztanó, Orsolya and Milovský, R and Hips, Kinga},
	doi = {10.1155/2020/9020684},
	journal-iso = {GEOFLUIDS},
	journal = {GEOFLUIDS},
	volume = {2020},
	unique-id = {31783545},
	issn = {1468-8115},
	year = {2020},
	eissn = {1468-8123},
	orcid-numbers = {Gier, S/0000-0002-7926-7714; Sztanó, Orsolya/0000-0003-0786-3653; Milovský, R/0000-0003-1880-865X; Hips, Kinga/0000-0003-2315-120X}
}

@article{MTMT:30899104,
	title = {Dolomitization of shallow-water, mixed silicilastic‑carbonate sequences: The Lower Triassic ramp succession of the Transdanubian Range, Hungary},
	url = {https://m2.mtmt.hu/api/publication/30899104},
	author = {Győri, Orsolya and Haas, János and Hips, Kinga and Lukoczki, Georgina and Budai, Tamás and Demény, Attila and Laczkó-Dobos, Emese},
	doi = {10.1016/j.sedgeo.2019.105549},
	journal-iso = {SEDIMENT GEOL},
	journal = {SEDIMENTARY GEOLOGY},
	volume = {395},
	unique-id = {30899104},
	issn = {0037-0738},
	abstract = {The Lower Triassic succession of the Transdanubian Range in Hungary comprises limestones, dolomite, marl, sandstones and siltstones, deposited in tidal flat, lagoon and ooid shoal environments on the marginal ramp of the western Neotethys. Seven cores were chosen for petrographic and stable isotope investigations aiming to reconstruct the paragenetic sequence with special regard to the dolomitization and hydrothermal events. Five lithotypes were differentiated: (i) dolomite, (ii) sandy, silty, clayey dolomite, and dolomarl, (iii), dolomitic siltstone and sandstone, (iv) dolomitic limestone, and (v) limestone. In these lithotypes, three types of dolomites are present: non-ferroan replacive, ferroan replacive, and ferroan cement. Fabric retentive and fabric destructive non-ferroan replacive dolomitization are interpreted to have occurred by seepage reflux. Supporting evidence includes the presence gypsum and anhydrite in the Lower Triassic beds. Stable isotope values of the ferroan dolomite (delta O-18 of -10.7 to -4.2 parts per thousand and delta C-13 of 4.8 to 4.7 parts per thousand) suggest dolomitization by fluids of relatively high temperature. The similar stable isotope values (delta O-18 of -9.3 to -5.8 parts per thousand and delta C-13 of -1.9 to 2.5 parts per thousand) of the non-ferroan dolomite phase suggest that the reflux dolomite was overprinted by this second dolomitization event. Traces of exotic minerals, such as barite, chalcopyrite, galena and sulphosalts were found as fillings of vugs and fractures in the dolomite-cemented sandstone. The metals could have been sourced from the underlying Permian red sandstone beds. The heterogeneous sediment composition had profound impact on the diagenesis of these sedimentary successions.},
	year = {2020},
	eissn = {1879-0968},
	orcid-numbers = {Győri, Orsolya/0000-0002-3646-9113; Haas, János/0000-0003-0929-8889; Hips, Kinga/0000-0003-2315-120X; Lukoczki, Georgina/0000-0002-0661-0198; Demény, Attila/0000-0003-0522-9018}
}

@CONFERENCE{MTMT:31156792,
	title = {Structural control on diagenesis: combined structural and isotope data on calcite cements of pre-rift clastic sediments in the Pannonian Basin},
	url = {https://m2.mtmt.hu/api/publication/31156792},
	author = {Beke, Barbara and Fodor, László and Laczkó-Dobos, Emese and Hips, Kinga},
	booktitle = {ILP 2019 :14th Workshop of the International Lithosphere Program Task Force Sedimentary Basins : abstracts},
	unique-id = {31156792},
	year = {2019},
	pages = {12-13},
	orcid-numbers = {Beke, Barbara/0000-0003-0797-1195; Hips, Kinga/0000-0003-2315-120X}
}

@article{MTMT:30417004,
	title = {Multiphase carbonate cementation in the Miocene Pétervására Sandstone (North Hungary): implications for basinal fluid flow and burial history},
	url = {https://m2.mtmt.hu/api/publication/30417004},
	author = {Laczkó-Dobos, Emese and Hips, Kinga},
	doi = {10.1515/geoca-2018-0030},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {69},
	unique-id = {30417004},
	issn = {1335-0552},
	year = {2018},
	eissn = {1336-8052},
	pages = {515-527},
	orcid-numbers = {Hips, Kinga/0000-0003-2315-120X}
}

@{MTMT:30354049,
	title = {Deformation bands in clastic sediments: their role in depth-temperature-time determinations and regional structural analysis},
	url = {https://m2.mtmt.hu/api/publication/30354049},
	author = {Fodor, László and Beke, Barbara and Laczkó-Dobos, Emese and Petrik, Attila and Hips, Kinga},
	booktitle = {Thermal and mechanical evolution of collisional and accretionary orogens},
	unique-id = {30354049},
	year = {2018},
	pages = {56-57},
	orcid-numbers = {Beke, Barbara/0000-0003-0797-1195; Hips, Kinga/0000-0003-2315-120X}
}

@{MTMT:3322778,
	title = {Structural diagenesis and carbonate cementation of Lower Miocene sandstone: Implications for basinal fluid flow and reservoir quality (Northern Hungary)},
	url = {https://m2.mtmt.hu/api/publication/3322778},
	author = {Laczkó-Dobos, Emese and Beke, Barbara and Hips, Kinga and Fodor, László},
	booktitle = {Geophysical research abstracts 20.},
	unique-id = {3322778},
	year = {2018},
	orcid-numbers = {Beke, Barbara/0000-0003-0797-1195; Hips, Kinga/0000-0003-2315-120X}
}

@CONFERENCE{MTMT:3240251,
	title = {Diagenetic evaluation of Pannonian lacustrine deposits in the MakóTrough, southeastern Hungary},
	url = {https://m2.mtmt.hu/api/publication/3240251},
	author = {Laczkó-Dobos, Emese and Rastislav, Milovský and Susanne, Gier and Hips, Kinga and Sztanó, Orsolya},
	booktitle = {EGU General Assembly 2017: Conference Abstracts},
	unique-id = {3240251},
	year = {2017},
	pages = {EGU2017-15054},
	orcid-numbers = {Hips, Kinga/0000-0003-2315-120X; Sztanó, Orsolya/0000-0003-0786-3653}
}