@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:33812365,
	title = {A Sirok környéki miocén rétegsor földtani és geomorfológiai reambulálása},
	url = {https://m2.mtmt.hu/api/publication/33812365},
	author = {Gál, Péter and Pecsmány, Péter and Petrik, Attila and Haranginé Lukács, Réka and Fodor, László and Kövér, Szilvia and Harangi, Szabolcs},
	booktitle = {Átalakulások},
	unique-id = {33812365},
	year = {2020},
	pages = {32.},
	orcid-numbers = {Pecsmány, Péter/0000-0002-6047-3286; Haranginé Lukács, Réka/0000-0002-2338-4209; Kövér, Szilvia/0000-0002-6736-4226; Harangi, Szabolcs/0000-0003-2372-4581}
}

@{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:30823166,
	title = {Age determination for valley networks on Mars using tectonic-fluvial interaction},
	url = {https://m2.mtmt.hu/api/publication/30823166},
	author = {Kereszturi, Ákos and Petrik, Attila},
	doi = {10.1016/j.pss.2019.104754},
	journal-iso = {PLANET SPACE SCI},
	journal = {PLANETARY AND SPACE SCIENCE},
	volume = {180},
	unique-id = {30823166},
	issn = {0032-0633},
	year = {2020},
	eissn = {1873-5088}
}

@article{MTMT:31099447,
	title = {The distribution of Pb, Cu and Zn in topsoil of the Campanian Region, Italy},
	url = {https://m2.mtmt.hu/api/publication/31099447},
	author = {Minolfi, Giulia and Petrik, Attila and Albanese, Stefano and Lima, Annamaria and Cannatelli, Claudia and Rezza, Carmela and De Vivo, Benedetto},
	doi = {10.1144/geochem2017-074},
	journal-iso = {GEOCHEM-EXPLOR ENV A},
	journal = {GEOCHEMISTRY-EXPLORATION ENVIRONMENT ANALYSIS},
	volume = {19},
	unique-id = {31099447},
	issn = {1467-7873},
	abstract = {In this paper we present a comparison of statistical and spatial distributions between Pb, Cu and Zn concentration data and clr-transformed data of 3669 topsoil samples from the Campanian Region. Results show that both approaches, the classical univariate analysis and the compositional data analysis, are necessary to understand the real structure of the data and shed light on different aspects. In particular, the spatial distributions of concentration ('raw') data and clr-transformed data of the three elements differ completely. Raw data essentially represent a high anthropogenic impact, requiring an additional human health risk assessment for the three investigated elements. The information obtained by the clr-coefficient maps reveals the geogenic contribution to the element distribution. To better constrain the degree of contamination due to these potentially toxic elements and their impact on human health, we present an RGB composite map of Pb, Cu and Zn. This map unravels potential sources of contamination and locates the areas where concentrations exceed thresholds established by the Italian legislation.},
	keywords = {CONTAMINATION; Compositional data; RGB; Campania; clr-transformation},
	year = {2019},
	eissn = {2041-4943},
	pages = {205-215}
}

@CONFERENCE{MTMT:30868741,
	title = {Geological and geomorphological remapping of the Miocene sedimentary-volcanic basin at the border area of the Mátra and Bükk Mountains (NE Hungary)},
	url = {https://m2.mtmt.hu/api/publication/30868741},
	author = {Gál, P. and Pecsmány, Péter and Petrik, Attila and Haranginé Lukács, Réka and Fodor, László and Kövér, Szilvia and Harangi, Szabolcs},
	booktitle = {ILP 2019 :14th Workshop of the International Lithosphere Program Task Force Sedimentary Basins : abstracts},
	unique-id = {30868741},
	year = {2019},
	pages = {32-34},
	orcid-numbers = {Pecsmány, Péter/0000-0002-6047-3286; Haranginé Lukács, Réka/0000-0002-2338-4209; Kövér, Szilvia/0000-0002-6736-4226; Harangi, Szabolcs/0000-0003-2372-4581}
}

@CONFERENCE{MTMT:30636043,
	title = {Deformation band formation in function of progressive burial: depth calibration and mechanism change in the Pannonian Basin (Hungary).},
	url = {https://m2.mtmt.hu/api/publication/30636043},
	author = {Beke, Barbara and Fodor, László and Petrik, Attila},
	booktitle = {Tectonic Studies Group Annual General Meeting},
	unique-id = {30636043},
	year = {2019},
	pages = {104},
	orcid-numbers = {Beke, Barbara/0000-0003-0797-1195}
}

@article{MTMT:30635811,
	title = {Deformation band formation as a function of progressive burial: Depth calibration and mechanism change in the Pannonian Basin (Hungary)},
	url = {https://m2.mtmt.hu/api/publication/30635811},
	author = {Beke, Barbara and Fodor, László and Millar, L and Petrik, Attila},
	doi = {10.1016/j.marpetgeo.2019.04.006},
	journal-iso = {MAR PETROL GEOL},
	journal = {MARINE AND PETROLEUM GEOLOGY},
	volume = {105},
	unique-id = {30635811},
	issn = {0264-8172},
	abstract = {Deformation bands (DB) are ubiquitous structural elements that can be found in Miocene pre- and syn-rift sediments of the extensional Pannonian Basin, central Europe. Across the field sites we see examples of disaggregation to cataclastic DB sets and evidence of frequent reactivation by discrete faulting. Thin section analysis, cross-cutting relationships and well-defined time constraints of analysed brittle structures demonstrate that with increased burial depth, DB deformation mechanisms progressed from granular flow to cataclasis.
		
		The DB sets were classified into 10 deformation phases based on formerly published independent fault-slip analysis and structural mapping. Subsidence curves were constructed for each stratigraphic level involved in deformation and were used along with the intersection of deformation episodes to calculate the depth intervals of DB generations and subsequent structural elements. The DB formation depths obtained were transferred to the depth range of the related mechanisms. This combined methodology permits a more quantitative approach to determine the changes in the deformation mechanisms with depth.
		
		Our results show that granular flow (disaggregation bands) dominates down to 100-150 m as the earliest deformation structure, followed by weak then moderate cataclasis. The transition between weak and moderate cataclasis is at approximately 300 +/- 100 m for host rock rich in feldspar or fragile tuffitic components and from around 900 +/- 100 m in quartz-rich sediments. In addition, deformation by frictional sliding concentrates on discrete fault planes at the margin of cataclastic bands or on new fracture planes from similar to 500 +/- 100 m in volcanoclastic or feldspar rich host rocks, and 1000 +/- 100 m in quartz-rich host rocks.
		
		We suggest that burial-induced diagenetic processes is dependent on subsidence history, and partly in connection with regional fluid migration path, control the transition from moderate or advanced cataclasis to discrete fault slip. All these changes affect the pore structure and porosity that contribute to rheological changes, and hence change in deformation mechanism of coeval fracturing events.},
	year = {2019},
	eissn = {1873-4073},
	pages = {1-16},
	orcid-numbers = {Beke, Barbara/0000-0003-0797-1195; Petrik, Attila/0000-0001-6164-1758}
}

@article{MTMT:30321155,
	title = {Variation in style of magmatism and emplacement mechanism induced by changes in basin environments and stress fields (Pannonian Basin, Central Europe)},
	url = {https://m2.mtmt.hu/api/publication/30321155},
	author = {Petrik, Attila and Fodor, László and Bereczki, László and Klembala, Zs and Haranginé Lukács, Réka and Baranyi, Viktória and Beke, Barbara and Harangi, Szabolcs},
	doi = {10.1111/bre.12326},
	journal-iso = {BASIN RES},
	journal = {BASIN RESEARCH},
	volume = {31},
	unique-id = {30321155},
	issn = {0950-091X},
	year = {2019},
	eissn = {1365-2117},
	pages = {380-404},
	orcid-numbers = {Haranginé Lukács, Réka/0000-0002-2338-4209; Baranyi, Viktória/0000-0002-1194-9903; Beke, Barbara/0000-0003-0797-1195; Harangi, Szabolcs/0000-0003-2372-4581}
}

@article{MTMT:30424852,
	title = {Spatial pattern recognition of arsenic in topsoil using high-density regional data},
	url = {https://m2.mtmt.hu/api/publication/30424852},
	author = {Petrik, Attila and Albanese, Stefano and Lima, Annamaria and Jordán, Győző and Rolandi, Roberto and Rezza, Carmela and De Vivo, Benedetto},
	doi = {10.1144/geochem2017-060},
	journal-iso = {GEOCHEM-EXPLOR ENV A},
	journal = {GEOCHEMISTRY-EXPLORATION ENVIRONMENT ANALYSIS},
	volume = {18},
	unique-id = {30424852},
	issn = {1467-7873},
	abstract = {Digital image processing analysis was carried out on As in topsoils of the Campania Region (Italy) to recognise any unknown spatial patterns. The highest As concentration is related to topsoils developed on the NW-SE-trending carbonate massifs overlain by pyroclastic rocks where the highest spatial variability and gradient magnitude of As concentration and the highest fault density were also observed. High As concentrations were also found in topsoils over volcanic rocks which played a control on its distribution pattern. The low As values are associated with topsoils along large fluvial valleys where the activity of rivers disturbed the As pattern by transporting larger grain-sized stream sediments with low As concentrations.},
	keywords = {Digital image processing; bedrock geology; fault density; terra rossa soils; Campania},
	year = {2018},
	eissn = {2041-4943},
	pages = {319-330}
}