TY - JOUR AU - Hips, Kinga TI - 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 JF - FACIES J2 - FACIES VL - 68 PY - 2022 IS - 3 PG - 17 SN - 0172-9179 DO - 10.1007/s10347-022-00646-3 UR - https://m2.mtmt.hu/api/publication/33524581 ID - 33524581 N1 - Cited By :1 Export Date: 6 February 2023 Correspondence Address: Hips, K.; MTA-ELTE Geological, Pázmány s. 1/c, Hungary; email: hips@staff.elte.hu AB - 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. LA - English DB - MTMT ER - TY - JOUR AU - Hips, Kinga TI - 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 JF - FACIES J2 - FACIES VL - 68 PY - 2022 IS - 3 SN - 0172-9179 DO - 10.1007/s10347-022-00646-3 UR - https://m2.mtmt.hu/api/publication/32794395 ID - 32794395 N1 - Funding Agency and Grant Number: Eotvos Lorand University Funding text: Open access funding provided by Eotvos Lorand University. LA - English DB - MTMT ER - TY - JOUR AU - Haas, János AU - Budai, Tamás AU - Hips, Kinga AU - Czuppon, György AU - Győri, Orsolya AU - Horváth, Anikó AU - Héja, Gábor TI - Dolomitization of Late Norian carbonate deposits of restricted basin facies in the Keszthely Mts., Transdanubian Range, Hungary JF - INTERNATIONAL JOURNAL OF EARTH SCIENCES J2 - INT J EARTH SCI VL - 111 PY - 2022 SP - 245 EP - 268 PG - 24 SN - 1437-3254 DO - 10.1007/s00531-021-02113-w UR - https://m2.mtmt.hu/api/publication/32490987 ID - 32490987 N1 - Department of Geology, Institute of Geography and Earth Sciences, Eötvös Loránd University, Pázmány P. sétány 1/c, Budapest, 1117, Hungary Mining and Geological Survey of Hungary, Stefánia út 14, Budapest, 1143, Hungary Geological, Geophysical and Space Science Research Group, Institute of Geography and Earth Sciences, Eötvös Loránd University, Pázmány Péter sétány 1/c, Budapest, 1117, Hungary Research Centre for Astronomy and Earth Sciences, Institute for Geological and Geochemical Research, Eötvös Loránd Research Network (ELKH), Budaörsi út 45, Budapest, 1112, Hungary TDE ITS Ltd, Pasaréti út 46, Budapest, 1026, Hungary Institute for Nuclear Research, Bem square 18c, Debrecen, 4026, Hungary Export Date: 15 February 2022 CODEN: IJESF Correspondence Address: Győri, O.; TDE ITS Ltd, Pasaréti út 46, Hungary; email: gyori.orsi@gmail.com AB - 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. LA - English DB - MTMT ER - 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 - 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 - Laczkó-Dobos, Emese AU - Gier, S AU - Sztanó, Orsolya AU - Milovský, R AU - Hips, Kinga TI - Porosity Development Controlled by Deep-Burial Diagenetic Process in Lacustrine Sandstones Deposited in a Back-Arc Basin (Makó Trough, Pannonian Basin, Hungary) JF - GEOFLUIDS J2 - GEOFLUIDS VL - 2020 PY - 2020 PG - 26 SN - 1468-8115 DO - 10.1155/2020/9020684 UR - https://m2.mtmt.hu/api/publication/31783545 ID - 31783545 N1 - Eötvös Loránd University, Pázmány Péter sétány 1/c, Budapest, 1117, Hungary MTA-ELTE Geological, Geophysical and Space Science Research Group, Pázmány P. sétány 1/c, Budapest, H -1117, Hungary Department of Geodynamics and Sedimentology, Universität Wien, Austria Earth Science Institute of the Slovak Academy of Sciences, Banská Bystrica, Ďumbierska, Slovakia Cited By :1 Export Date: 4 July 2022 Correspondence Address: Laczkó-Dobos, E.; Eötvös Loránd University, Pázmány Péter sétány 1/c, Hungary; email: meseszocs@caesar.elte.hu LA - English DB - MTMT ER - TY - JOUR AU - Hips, Kinga AU - Haas, János AU - Szilágyi, Zsanett TI - Mikrobialitok jellegzetességei: a biofilmek szerepe a karbonátkiválásban JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 150 PY - 2020 IS - 3 SP - 397 EP - 422 PG - 26 SN - 0015-542X DO - 10.23928/foldt.kozl.2020.150.3.397 UR - https://m2.mtmt.hu/api/publication/31620714 ID - 31620714 N1 - MTA–ELTE Geológiai, Geofizikai és Űrtudományi Kutatócsoport, Pázmány Péter sétány 1/C, Budapest, 1117, Hungary The University of Sydney, Geocoastal Research Group, Madsen Building F09, Camperdown, NSW 2006, Australia Export Date: 19 May 2022 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Szilágyi, Zsanett AU - Webster, Jody M. AU - Patterson, Madhavi A. AU - Hips, Kinga AU - Riding, Robert AU - Foley, Matthew AU - Humblet, Marc AU - Yokoyama, Yusuke AU - Liang, Liyuan AU - Gischler, Eberhard AU - Montaggioni, Lucien AU - Gherardi, Douglas AU - Braga, Juan C. TI - Controls on the spatio-temporal distribution of microbialite crusts on the Great Barrier Reef over the past 30,000 years JF - MARINE GEOLOGY J2 - MAR GEOL VL - 429 PY - 2020 SN - 0025-3227 DO - 10.1016/j.margeo.2020.106312 UR - https://m2.mtmt.hu/api/publication/31525966 ID - 31525966 LA - English DB - MTMT ER - TY - JOUR AU - Haas, János AU - Hips, Kinga TI - A rejtelmes dolomit JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 150 PY - 2020 IS - 2 SP - 233 EP - 266 PG - 34 SN - 0015-542X DO - 10.23928/foldt.kozl.2020.150.2.233 UR - https://m2.mtmt.hu/api/publication/31372620 ID - 31372620 N1 - Cited By :1 Export Date: 4 January 2023 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Győri, Orsolya AU - Haas, János AU - Hips, Kinga AU - Lukoczki, Georgina AU - Budai, Tamás AU - Demény, Attila AU - Laczkó-Dobos, Emese TI - Dolomitization of shallow-water, mixed silicilastic‑carbonate sequences: The Lower Triassic ramp succession of the Transdanubian Range, Hungary JF - SEDIMENTARY GEOLOGY J2 - SEDIMENT GEOL VL - 395 PY - 2020 PG - 20 SN - 0037-0738 DO - 10.1016/j.sedgeo.2019.105549 UR - https://m2.mtmt.hu/api/publication/30899104 ID - 30899104 N1 - MTA-ELTE Geological, Geophysical and Space Science Research Group, Pázmány P. sétány 1/c, Budapest, H–1117, Hungary Department of Physical and Applied Geology, Eötvös Loránd University, Pázmány P. sétány 1/c, Budapest, H–1117, Hungary University of Kentucky, Kentucky Geological Survey, Mining and Mineral Resources Building, Lexington, KY 40506, United States Department of Geology and Meteorology, University of Pécs, 7624 Ifjúság útja 6, Pécs, Hungary Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi street 45, Budapest, H-1112, Hungary Cited By :5 Export Date: 30 June 2022 Correspondence Address: Győri, O.; MTA-ELTE Geological, Pázmány P. sétány 1/c, Hungary; email: gyoriorsolya@caesar.elte.hu AB - 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. LA - English DB - MTMT ER -