@article{MTMT:33524581,
	title = {Sedimentary aspects of the onset of Middle Triassic continental rifting in the western end of Neotethys; inferences from the Silica and Torna Nappes, NE Hungary: a review},
	url = {https://m2.mtmt.hu/api/publication/33524581},
	author = {Hips, Kinga},
	doi = {10.1007/s10347-022-00646-3},
	journal-iso = {FACIES},
	journal = {FACIES},
	volume = {68},
	unique-id = {33524581},
	issn = {0172-9179},
	abstract = {The initiation of continental rifting from the latest Early Triassic was reconstructed by correlation of sedimentary formations deposited in the western end of Neotethys (in the Dinaric-Alpine oceanic branch). The shallow-marine and basinal strata of the Silica Nappes and the Bodvarako Series from the Torna Nappe (located in the southern part of the Inner Western Carpathians) were studied and compared to sedimentary successions described from the Alps, the Carpathians and the Dinarides. The depositional zonation, developed on the shelf during the Late Permian-Early Triassic transgression, was dissected and rearranged from the latest Early Triassic. The facies pattern and the differential sedimentary evolution of the shelf domains suggest that the accelerated subsidence began in the latest Early Triassic, and was connected to the onset of continental rifting. Three stages are reconstructed in the studied time-frame. (1) Dark grey carbonates, very poor in fossils, were deposited in restricted and hypersaline intraplatform basins in many shelf domains. In the external domains, shallow-marine carbonates, depositional gaps and terrestrial deposits are typical (formations in the Southern Alps, the External Dinarides and the Serbian-Macedonian Massif). From the latest Early Triassic, this latter shelf segment formed a threshold that restricted water circulation from the intraplatform basins. (2) Shallowing-up carbonate successions mark the next stage that implies a period of tectonic quiescence on the shelf from the late Early Anisian to late Middle Anisian. A peculiar change in biota occurring in previously restricted domains was coeval in shallow-marine and deep-marine settings. The biotic change is revealed by observations that dark grey carbonates, which are very poor in fossils, are overlain by carbonate successions rich in fossils typical for normal-marine water. The biota and environmental changes indicate the opening of a passage which allowed the circulation of well-oxygenated and normal-salinity marine water towards the previously restricted depositional areas. The geodynamic setting switching from continental rifting to spreading in the southern sector of the Dinaric-Alpine oceanic branch (Hellenides and Albanides), triggered the opening of the gateway between the future continental margins, i.e., between the External Dinaridic domain (Adria) and Serbian-Macedonian Massif (Eurasia). (3) Following the biotic event in the northern sector of the shelf, subsidence accelerated and additional intraplatform basins opened from the latest Pelsonian.},
	keywords = {Carbonates; GEODYNAMIC EVOLUTION; Microbialites; Extensional setting; Biotic changes; Facies correlation},
	year = {2022},
	eissn = {1612-4820},
	orcid-numbers = {Hips, Kinga/0000-0003-2315-120X}
}

@article{MTMT:32794395,
	title = {Sedimentary aspects of the onset of Middle Triassic continental rifting in the western end of Neotethys; inferences from the Silica and Torna Nappes, NE Hungary: a review},
	url = {https://m2.mtmt.hu/api/publication/32794395},
	author = {Hips, Kinga},
	doi = {10.1007/s10347-022-00646-3},
	journal-iso = {FACIES},
	journal = {FACIES},
	volume = {68},
	unique-id = {32794395},
	issn = {0172-9179},
	year = {2022},
	eissn = {1612-4820},
	orcid-numbers = {Hips, Kinga/0000-0003-2315-120X}
}

@article{MTMT:32490987,
	title = {Dolomitization of Late Norian carbonate deposits of restricted basin facies in the Keszthely Mts., Transdanubian Range, Hungary},
	url = {https://m2.mtmt.hu/api/publication/32490987},
	author = {Haas, János and Budai, Tamás and Hips, Kinga and Czuppon, György and Győri, Orsolya and Horváth, Anikó and Héja, Gábor},
	doi = {10.1007/s00531-021-02113-w},
	journal-iso = {INT J EARTH SCI},
	journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
	volume = {111},
	unique-id = {32490987},
	issn = {1437-3254},
	abstract = {In the Transdanubian Range (Hungary), a wide spectrum of Triassic dolomites is known. Mechanism of dolomitization of the platform carbonate successions was subject of a number of studies but the study of dolomitization of basinal carbonates is very limited. Petrographical and isotope-geochemical characteristics of the Upper Triassic dolomitized carbonate deposits, formed in a fault-controlled intraplatform basin, and interpretation of the dolomite-forming processes are presented in the current paper. From the latest Carnian to Middle Norian under semi-arid climatic conditions density-driven flux of seawater derived mesohaline fluids was the dominant mechanism of the near-surface pervasive dolomitization of the thick platform carbonate succession. In the late Middle Norian incipient rifting of the Alpine Tethys led to establishment of an extensional structural regime and onset of the formation of the Kossen Basin. In the study area, above the dolomitized platform carbonate succession, platform-derived carbonate sediments were accumulated in a fault-bounded, semi-restricted sub-basin of the Kossen Basin, whereas talus breccias and debrites were deposited near a basin-bounding master fault. The basin deposits (lower and upper members of the Rezi Dolomite Formation) were subject of early diagenetic dolomitization in shallow burial setting. Enhanced salinity seawater was the dolomitizing fluid; the synsedimentary fracturing may have promoted the fluid flow and thereby the dolomitization. Thick-bedded carbonates (middle member of the Rezi Dolomite Formation) representing a progradational tongue of the ambient platform are intercalated between the basin deposits. The dolomitization of this unit can be explained by the reflux model.},
	year = {2022},
	eissn = {1437-3262},
	pages = {245-268},
	orcid-numbers = {Haas, János/0000-0003-0929-8889; Hips, Kinga/0000-0003-2315-120X; Czuppon, György/0000-0002-7231-6042; Győri, Orsolya/0000-0002-3646-9113}
}

@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}
}

@{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:31620714,
	title = {Mikrobialitok jellegzetességei: a biofilmek szerepe a karbonátkiválásban},
	url = {https://m2.mtmt.hu/api/publication/31620714},
	author = {Hips, Kinga and Haas, János and Szilágyi, Zsanett},
	doi = {10.23928/foldt.kozl.2020.150.3.397},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {150},
	unique-id = {31620714},
	issn = {0015-542X},
	year = {2020},
	eissn = {2559-902X},
	pages = {397-422},
	orcid-numbers = {Hips, Kinga/0000-0003-2315-120X; Haas, János/0000-0003-0929-8889; Szilágyi, Zsanett/0000-0001-6271-0153}
}

@article{MTMT:31525966,
	title = {Controls on the spatio-temporal distribution of microbialite crusts on the Great Barrier Reef over the past 30,000 years},
	url = {https://m2.mtmt.hu/api/publication/31525966},
	author = {Szilágyi, Zsanett and Webster, Jody M. and Patterson, Madhavi A. and Hips, Kinga and Riding, Robert and Foley, Matthew and Humblet, Marc and Yokoyama, Yusuke and Liang, Liyuan and Gischler, Eberhard and Montaggioni, Lucien and Gherardi, Douglas and Braga, Juan C.},
	doi = {10.1016/j.margeo.2020.106312},
	journal-iso = {MAR GEOL},
	journal = {MARINE GEOLOGY},
	volume = {429},
	unique-id = {31525966},
	issn = {0025-3227},
	year = {2020},
	eissn = {1872-6151},
	orcid-numbers = {Szilágyi, Zsanett/0000-0001-6271-0153; Hips, Kinga/0000-0003-2315-120X}
}

@article{MTMT:31372620,
	title = {A rejtelmes dolomit},
	url = {https://m2.mtmt.hu/api/publication/31372620},
	author = {Haas, János and Hips, Kinga},
	doi = {10.23928/foldt.kozl.2020.150.2.233},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {150},
	unique-id = {31372620},
	issn = {0015-542X},
	year = {2020},
	eissn = {2559-902X},
	pages = {233-266},
	orcid-numbers = {Haas, János/0000-0003-0929-8889; 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}
}