TY - JOUR AU - Beke, Barbara AU - Laczkó-Dobos, Emese AU - Hips, Kinga AU - Schubert, Félix AU - Petrik, Attila AU - Milovský, R AU - Fodor, László TI - Evolution of deformation mechanism and fluid flow in two pre-rift siliciclastic deposits (Pannonian Basin, Hungary) JF - GLOBAL AND PLANETARY CHANGE J2 - GLOBAL PLANET CHANGE VL - 199 PY - 2021 SN - 0921-8181 DO - 10.1016/j.gloplacha.2021.103434 UR - https://m2.mtmt.hu/api/publication/31850039 ID - 31850039 N1 - MTA-ELTE Geological, Geophysical and Space Science Research Group, Pázmány P. sétány 1/C, Budapest, 1117, Hungary Department of Mineralogy, Geochemistry and Petrology, University of Szeged, Egyetem utca 2-6, Szeged, 6702, Hungary Eriksfiord AS, Prof. Olav Hanssensvei 7A, Stavanger, 4021, Norway Slovak Academy of Sciences, Earth Science Institute, Ďumbierska 1, Banská Bystrica, SK-974 01, Slovakia Eötvös Loránd University, Department of Physical and Applied Geology, Pázmány P. sétány 1/C, Budapest, 1117, Hungary Cited By :3 Export Date: 11 July 2022 CODEN: GPCHE Correspondence Address: Beke, B.; MTA-ELTE Geological, Pázmány P. sétány 1/C, Hungary; email: barbara.beke@gmail.com LA - English DB - MTMT ER - TY - CHAP AU - Gál, Péter AU - Pecsmány, Péter AU - Petrik, Attila AU - Haranginé Lukács, Réka AU - Fodor, László AU - Kövér, Szilvia AU - Harangi, Szabolcs ED - Füri, Judit Izabella ED - Király, Edit TI - A Sirok környéki miocén rétegsor földtani és geomorfológiai reambulálása T2 - Átalakulások PB - Magyar Bányászati és Földtani Szolgálat CY - Budapest SN - 9789636713201 PY - 2020 SP - 32. UR - https://m2.mtmt.hu/api/publication/33812365 ID - 33812365 LA - Hungarian DB - MTMT ER - TY - CHAP AU - Beke, Barbara AU - Laczkó-Dobos, Emese AU - Hips, Kinga AU - Schubert, Félix AU - Petrik, Attila AU - Fodor, László ED - Füri, Judit Izabella ED - Király, Edit TI - Szerkezeti elemek és a diagenezis kapcsolata porózus, sziliciklasztos üledékekben ÉK-magyarországon. T2 - Átalakulások PB - Magyar Bányászati és Földtani Szolgálat CY - Budapest SN - 9789636713201 PY - 2020 SP - 19 PG - 2 UR - https://m2.mtmt.hu/api/publication/31936889 ID - 31936889 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Kereszturi, Ákos AU - Petrik, Attila TI - Age determination for valley networks on Mars using tectonic-fluvial interaction JF - PLANETARY AND SPACE SCIENCE J2 - PLANET SPACE SCI VL - 180 PY - 2020 SN - 0032-0633 DO - 10.1016/j.pss.2019.104754 UR - https://m2.mtmt.hu/api/publication/30823166 ID - 30823166 N1 - Research Center for Astronomy and Earth Sciences, Konkoly Astronomical Institute, Konkoly Thege Miklos Street 15-17, Budapest, H-1121, Hungary Hungarian Astronomy Non-profit Ltd. (MCSN Kft), Hungary Department of Physical and Applied Geology, Eötvös University, Budapest, Hungary Export Date: 30 September 2019 CODEN: PLSSA Correspondence Address: Kereszturi, A.; Research Center for Astronomy and Earth Sciences, Konkoly Astronomical Institute, Konkoly Thege Miklos street 15-17, Hungary; email: kereszturi.akos@csfk.mta.hu Funding Agency and Grant Number: Excellence of Strategic R&D centres project of NKFIH [GINOP-2.3.2-15-2016-00003]; H2020 fund; [COOP-NN-116927] Funding text: The crater forming impact rate analysis was supported by the Excellence of Strategic R&D centres (GINOP-2.3.2-15-2016-00003) project of NKFIH and the related H2020 fund, and the Mars analog characteristics on the Earth were supported by the COOP-NN-116927 project. The consultation with Jordan Gyozo is acknowledged. LA - English DB - MTMT ER - TY - JOUR AU - Minolfi, Giulia AU - Petrik, Attila AU - Albanese, Stefano AU - Lima, Annamaria AU - Cannatelli, Claudia AU - Rezza, Carmela AU - De Vivo, Benedetto TI - The distribution of Pb, Cu and Zn in topsoil of the Campanian Region, Italy JF - GEOCHEMISTRY-EXPLORATION ENVIRONMENT ANALYSIS J2 - GEOCHEM-EXPLOR ENV A VL - 19 PY - 2019 IS - 3 SP - 205 EP - 215 PG - 11 SN - 1467-7873 DO - 10.1144/geochem2017-074 UR - https://m2.mtmt.hu/api/publication/31099447 ID - 31099447 AB - 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. LA - English DB - MTMT ER - TY - CONF AU - Gál, P. AU - Pecsmány, Péter AU - Petrik, Attila AU - Haranginé Lukács, Réka AU - Fodor, László AU - Kövér, Szilvia AU - Harangi, Szabolcs ED - Kövér, Szilvia TI - Geological and geomorphological remapping of the Miocene sedimentary-volcanic basin at the border area of the Mátra and Bükk Mountains (NE Hungary) T2 - ILP 2019 :14th Workshop of the International Lithosphere Program Task Force Sedimentary Basins : abstracts C1 - Hévíz PY - 2019 SP - 32 EP - 34 PG - 3 UR - https://m2.mtmt.hu/api/publication/30868741 ID - 30868741 LA - English DB - MTMT ER - TY - CONF AU - Beke, Barbara AU - Fodor, László AU - Petrik, Attila TI - Deformation band formation in function of progressive burial: depth calibration and mechanism change in the Pannonian Basin (Hungary). T2 - Tectonic Studies Group Annual General Meeting PY - 2019 SP - 104 UR - https://m2.mtmt.hu/api/publication/30636043 ID - 30636043 LA - English DB - MTMT ER - TY - JOUR AU - Beke, Barbara AU - Fodor, László AU - Millar, L AU - Petrik, Attila TI - Deformation band formation as a function of progressive burial: Depth calibration and mechanism change in the Pannonian Basin (Hungary) JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 105 PY - 2019 SP - 1 EP - 16 PG - 16 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2019.04.006 UR - https://m2.mtmt.hu/api/publication/30635811 ID - 30635811 N1 - MTA-ELTE Geological Geophysical and Space Science Research Group, Pázmány Sétány 1/C, Budapest, H-1117, Hungary MTA-ELTE Volcanology Research Group, Pázmány Péter Sétány 1/C, Budapest, H-1117, Hungary Department of Civil and Environmental Engineering, University of Strathclyde, Glasgow, United Kingdom Cited By :2 Export Date: 27 November 2019 Correspondence Address: Beke, B.; MTA-ELTE Geological Geophysical and Space Science Research Group, Pázmány Sétány 1/C, Hungary; email: barbara.beke@gmail.com AB - 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. LA - English DB - MTMT ER - TY - JOUR AU - Petrik, Attila AU - Fodor, László AU - Bereczki, László AU - Klembala, Zs AU - Haranginé Lukács, Réka AU - Baranyi, Viktória AU - Beke, Barbara AU - Harangi, Szabolcs TI - Variation in style of magmatism and emplacement mechanism induced by changes in basin environments and stress fields (Pannonian Basin, Central Europe) JF - BASIN RESEARCH J2 - BASIN RES VL - 31 PY - 2019 IS - 2 SP - 380 EP - 404 PG - 25 SN - 0950-091X DO - 10.1111/bre.12326 UR - https://m2.mtmt.hu/api/publication/30321155 ID - 30321155 LA - English DB - MTMT ER - TY - JOUR AU - Petrik, Attila AU - Albanese, Stefano AU - Lima, Annamaria AU - Jordán, Győző AU - Rolandi, Roberto AU - Rezza, Carmela AU - De Vivo, Benedetto TI - Spatial pattern recognition of arsenic in topsoil using high-density regional data JF - GEOCHEMISTRY-EXPLORATION ENVIRONMENT ANALYSIS J2 - GEOCHEM-EXPLOR ENV A VL - 18 PY - 2018 IS - 4 SP - 319 EP - 330 PG - 12 SN - 1467-7873 DO - 10.1144/geochem2017-060 UR - https://m2.mtmt.hu/api/publication/30424852 ID - 30424852 N1 - Department of Earth, Environment and Resources Sciences, University of Naples Federico II, Via Cintia snc, Naples, 80126, Italy Department of Applied Geochemistry, Szent István University, Gödöllő, Hungary Pegaso University, Piazza Trieste e Trento 48, Napoli, 80132, Italy Environment and Territory Department, Benecon Scarl, Via S. Maria di Costantinopoli 104, Naples, 80138, Italy Cited By :3 Export Date: 5 February 2020 Correspondence Address: Petrik, A.; Department of Earth, Environment and Resources Sciences, University of Naples Federico II, Via Cintia snc, Italy; email: petrik.atus@gmail.com AB - 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. LA - English DB - MTMT ER -