Dunkl, István

[["dc.bibliographiccitation.firstpage","121"],["dc.bibliographiccitation.journal","Sedimentary Geology"],["dc.bibliographiccitation.lastpage","126"],["dc.bibliographiccitation.volume","389"],["dc.contributor.author","Stalder, Roland"],["dc.contributor.author","von Eynatten, Hilmar"],["dc.contributor.author","Costamoling, Julian"],["dc.contributor.author","Potrafke, Alexander"],["dc.contributor.author","Dunkl, István"],["dc.contributor.author","Meinhold, Guido"],["dc.date.accessioned","2020-12-10T15:21:17Z"],["dc.date.available","2020-12-10T15:21:17Z"],["dc.date.issued","2019"],["dc.identifier.doi","10.1016/j.sedgeo.2019.06.001"],["dc.identifier.issn","0037-0738"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/16767"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/72975"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.notes.intern","Merged from goescholar"],["dc.rights","CC BY-NC-ND 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by-nc-nd/4.0"],["dc.title","OH in detrital quartz grains as tool for provenance analysis: Case studies on various settings from Cambrian to Recent"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1557"],["dc.bibliographiccitation.issue","5"],["dc.bibliographiccitation.journal","International Journal of Earth Sciences"],["dc.bibliographiccitation.lastpage","1580"],["dc.bibliographiccitation.volume","106"],["dc.contributor.author","Heberer, Bianca"],["dc.contributor.author","Reverman, Rebecca Lee"],["dc.contributor.author","Fellin, Maria Giuditta"],["dc.contributor.author","Neubauer, Franz"],["dc.contributor.author","Dunkl, Istvan"],["dc.contributor.author","Zattin, Massimiliano"],["dc.contributor.author","Seward, Diane"],["dc.contributor.author","Genser, Johann"],["dc.contributor.author","Brack, Peter"],["dc.date.accessioned","2018-11-07T10:22:10Z"],["dc.date.available","2018-11-07T10:22:10Z"],["dc.date.issued","2017"],["dc.description.abstract","Indentation of rigid blocks into rheologically weak orogens is generally associated with spatiotemporally variable vertical and lateral block extrusion. The European Eastern and Southern Alps are a prime example of microplate indentation, where most of the deformation was accommodated north of the crustal indenter within the Tauern Window. However, outside of this window only the broad late-stage exhumation pattern of the indented units as well as of the indenter itself is known. In this study we refine the exhumational pattern with new (U-Th-Sm)/He and fission-track thermochronology data on apatite from the Karawanken Mountains adjacent to the eastern Periadriatic fault and from the central-eastern Southern Alps. Apatite (U-Th-Sm)/He ages from the Karawanken Mountains range between 12 and 5 Ma and indicate an episode of fault-related exhumation leading to the formation of a positive flower structure and an associated peripheral foreland basin. In the Southern Alps, apatite (U-Th-Sm)/He and fission-track data combined with previous data also indicate a pulse of mainly Late Miocene exhumation, which was maximized along thrust systems, with highly differential amounts of displacement along individual structures. Our data contribute to mounting evidence for widespread Late Miocene tectonic activity, which followed a phase of major exhumation during strain localization in the Tauern Window. We attribute this exhumational phase and more distributed deformation during Adriatic indentation to a major change in boundary conditions operating on the orogen, likely due to a shift from a decoupled to a coupled system, possibly enhanced by a shift in convergence direction."],["dc.identifier.doi","10.1007/s00531-016-1367-3"],["dc.identifier.isi","000403982300007"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/14180"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/42230"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","PUB_WoS_Import"],["dc.publisher","Springer"],["dc.relation.issn","1437-3262"],["dc.relation.issn","1437-3254"],["dc.rights","CC BY 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0/"],["dc.title","Postcollisional cooling history of the Eastern and Southern Alps and its linkage to Adria indentation"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","275"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","Andean Geology"],["dc.bibliographiccitation.volume","44"],["dc.contributor.author","Bense, Frithjof"],["dc.contributor.author","Costa, Carlos"],["dc.contributor.author","Oriolo, Sebastián"],["dc.contributor.author","Löbens, Stefan"],["dc.contributor.author","Dunkl, Istvan"],["dc.contributor.author","Wemmer, Klaus"],["dc.contributor.author","Siegesmund, Siegfried"],["dc.date.accessioned","2020-12-10T18:47:50Z"],["dc.date.available","2020-12-10T18:47:50Z"],["dc.date.issued","2017"],["dc.identifier.doi","10.5027/andgeoV44n3-a03"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/14893"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/78909"],["dc.notes.intern","DOI Import GROB-354"],["dc.notes.intern","Merged from goescholar"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.rights","CC BY 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0/"],["dc.title","Exhumation history and landscape evolution of the Sierra de San Luis (Sierras Pampeanas, Argentina) - new insights from low - temperature thermochronological data"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","133"],["dc.bibliographiccitation.issue","102"],["dc.bibliographiccitation.journal","Austrian Journal of Earth Sciences [untranslated]"],["dc.bibliographiccitation.lastpage","145"],["dc.contributor.author","Dunkl, István"],["dc.contributor.author","Schuller, Volker"],["dc.contributor.author","Frisch, Wolfgang"],["dc.contributor.author","DANIŠÍK, Martin"],["dc.contributor.author","Melinte, Mihaela Carmen"],["dc.date.accessioned","2019-07-10T08:13:24Z"],["dc.date.available","2019-07-10T08:13:24Z"],["dc.date.issued","2009"],["dc.description.abstract","The Apuseni Mountains were formed during Late Cretaceous convergence between the Tisia and the Dacia microplates as part of the Alpine orogen. The mountain range comprises a sedimentary succession similar to the Gosau Group of the Eastern Alps. This work focuses on the sedimentological and geodynamic evolution of the Gosau basin of the Apuseni Mts. and attempts a direct comparison to the relatively well studied Gosau Group deposits of the Eastern Alps. By analyzing the Upper Cretaceous Gosau sediments and the surrounding geological units, we were able to add critical evidence for reconstructing the Late Mesozoic to Paleogene geodynamic evolution of the Apuseni Mountains. Nannoplankton investigations show that Gosau sedimentation started diachronously after Late Turonian times. The burial history indicates low subsidence rates during deposition of the terrestrial and shallow marine Lower Gosau Subgroup and increased subsidence rates during the period of deep marine Upper Gosau Subgroup sedimentation. The Gosau Group of the Apuseni Mountains was deposited in a forearc basin supplied with sedimentary material from an obducted forearc region and the crystalline hinterland, as reflected by heavy mineral and paleocurrent analysis. Zircon fission track age populations show no fluctuation of exhumation rates in the surrounding geological units, which served as source areas for the detrital material, whereas increased exhumation at the K/Pg boundary can be proven by thermal modeling on apatite fission track data. Synchronously to the Gosau sedimentation, deep marine turbidites were deposited in the deep-sea trench basin formed by the subduction of the Transylvanian Ocean. The similarities to the Gosau occurrences of the Eastern Alps lead to direct correlation with the Alpine paleogeographic evolution and to the assumption that a continuous ocean basin (South Penninic - Transylvanian Ocean Basin) was consumed until Late Cretaceous times."],["dc.identifier.fs","502852"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/5923"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/61234"],["dc.language.iso","en"],["dc.notes.intern","Merged from goescholar"],["dc.relation.issn","0251-7493"],["dc.relation.orgunit","Fakultät für Geowissenschaften und Geographie"],["dc.rights","Goescholar"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.subject.ddc","550"],["dc.title","Upper Cretaceous Gosau deposits of the Apuseni Mountains (Romania) - similarities and differences to the Eastern Alps"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","385"],["dc.bibliographiccitation.issue","7"],["dc.bibliographiccitation.journal","Minerals"],["dc.bibliographiccitation.volume","9"],["dc.contributor.author","Lünsdorf, Nils Keno"],["dc.contributor.author","Kalies, Jannick"],["dc.contributor.author","Ahlers, Patrick"],["dc.contributor.author","Dunkl, István"],["dc.contributor.author","von Eynatten, Hilmar"],["dc.date.accessioned","2020-12-10T18:47:16Z"],["dc.date.available","2020-12-10T18:47:16Z"],["dc.date.issued","2019"],["dc.identifier.doi","10.3390/min9070385"],["dc.identifier.eissn","2075-163X"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/16578"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/78700"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.notes.intern","Merged from goescholar"],["dc.publisher","MDPI"],["dc.relation.eissn","2075-163X"],["dc.rights","CC BY 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0"],["dc.title","Semi-Automated Heavy-Mineral Analysis by Raman Spectroscopy"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","935"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","Solid Earth"],["dc.bibliographiccitation.lastpage","958"],["dc.bibliographiccitation.volume","12"],["dc.contributor.author","von Eynatten, Hilmar"],["dc.contributor.author","Kley, Jonas"],["dc.contributor.author","Dunkl, István"],["dc.contributor.author","Hoffmann, Veit-Enno"],["dc.contributor.author","Simon, Annemarie"],["dc.date.accessioned","2021-06-01T09:42:44Z"],["dc.date.available","2021-06-01T09:42:44Z"],["dc.date.issued","2021"],["dc.description.abstract","Abstract. Large parts of central Europe experienced exhumation in Late Cretaceous to Paleogene time. Previous studies mainly focused on thrusted basement uplifts to unravel the magnitude, processes and timing of exhumation. This study provides, for the first time, a comprehensive thermochronological dataset from mostly Permo-Triassic strata exposed adjacent to and between the basement uplifts in central Germany, comprising an area of at least some 250–300 km across. Results of apatite fission-track and (U–Th) / He analyses on > 100 new samples reveal that (i) kilometre-scale exhumation affected the entire region, (ii) thrusting of basement blocks like the Harz Mountains and the Thuringian Forest focused in the Late Cretaceous (about 90–70 Ma), while superimposed domal uplift of central Germany is slightly younger (about 75–55 Ma), and (iii) large parts of the domal uplift experienced removal of 3 to 4 km of Mesozoic strata. Using spatial extent, magnitude and timing as constraints suggests that thrusting and crustal thickening alone can account for no more than half of the domal uplift. Most likely, dynamic topography caused by upwelling asthenosphere significantly contributed to the observed pattern of exhumation in central Germany."],["dc.description.sponsorship","Open-Access-Publikationsfonds 2021"],["dc.identifier.doi","10.5194/se-12-935-2021"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/85337"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-425"],["dc.relation.eissn","1869-9529"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.rights","CC BY 4.0"],["dc.title","Late Cretaceous to Paleogene exhumation in central Europe – localized inversion vs. large-scale domal uplift"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","7443"],["dc.bibliographiccitation.issue","11"],["dc.bibliographiccitation.journal","Geological Journal"],["dc.bibliographiccitation.lastpage","7457"],["dc.bibliographiccitation.volume","55"],["dc.contributor.author","Zhou, Jianping"],["dc.contributor.author","Dunkl, István"],["dc.contributor.author","Liu, Yongjiang"],["dc.contributor.author","Li, Weimin"],["dc.contributor.author","Wolf, Anna"],["dc.contributor.author","von Eynatten, Hilmar"],["dc.date.accessioned","2021-04-14T08:26:17Z"],["dc.date.available","2021-04-14T08:26:17Z"],["dc.date.issued","2020"],["dc.description.abstract","Mafic lavas of Cenozoic age are widely distributed in northeast China and received much attention as an important part of the Circum‐Pacific volcanic belt. The age constraints for the volcanic activity were determined mostly by K/Ar and 40Ar/39Ar methods. We present zircon (U–Th)/He ages obtained on the thermally overprinted sands directly underlying a basaltic lava. This thermochronometer is insensitive to weathering and not biased by excess argon, thus it can express accurately the age of thermal effect of the lava flow. As a regional cooling age reference, three granite samples were dated from basement units that have not been thermally influenced by the basalt eruptions. The reference granite samples revealed well‐defined Cretaceous (U–Th)/He‐ages, while 20 zircon crystals from the sand below the basalt lava revealed a prominent Miocene (U–Th)/He age component of 9.33 ± 0.24 Ma. Raman spectroscopy of these zircon crystals supports their thermally overprinted character. We infer that the sand sample has experienced significant thermal overprint by the overlying basalt lava leading to thermal reset of the majority of the detrital zircon crystals. The obtained age is thus interpreted as the eruption age of the basalt lava. The Huanan basalt flow thus belongs to volcanics of the Laoyeling episode in NE China."],["dc.description.sponsorship","China Scholarship Council http://dx.doi.org/10.13039/501100004543"],["dc.description.sponsorship","National Key R\\u0026D Program of China"],["dc.description.sponsorship","Qingdao Leading innovation talents"],["dc.description.sponsorship","Taishan Scholars"],["dc.identifier.doi","10.1002/gj.3877"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/81890"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-399"],["dc.publisher","John Wiley \\u0026 Sons, Inc."],["dc.relation.eissn","1099-1034"],["dc.relation.issn","0072-1050"],["dc.rights","This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited."],["dc.title","Miocene age of the Huanan basalt lava flow (NE China) inferred by reset of zircon (U–Th)/He thermochronometer in the underlying sand"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1"],["dc.bibliographiccitation.journal","International Journal of Earth Sciences"],["dc.bibliographiccitation.lastpage","16"],["dc.contributor.author","Dunkl, István"],["dc.contributor.author","Farics, Éva"],["dc.contributor.author","Józsa, Sándor"],["dc.contributor.author","Lukács, Réka"],["dc.contributor.author","Haas, János"],["dc.contributor.author","Budai, Tamás"],["dc.date.accessioned","2019-07-09T11:51:36Z"],["dc.date.available","2019-07-09T11:51:36Z"],["dc.date.issued","2019"],["dc.description.abstract","The South Alpine–Dinaridic realm was affected by igneous activity in the Middle Triassic; the marine carbonate platforms and the adjacent basins contain highly variable intrusive-volcanic assemblages. We studied the petrography and determined the zircon U–Pb ages of the Triassic volcanic products in the Transdanubian Range. The geochemical features and thus the geodynamic context of the magmatism are badly known, as the rocks experienced variable chemical alteration. The exact duration of the igneous activity is also poorly constrained, as the geochronological data of the former studies were obtained mostly by the weathering-sensitive K–Ar and Rb–Sr methods and thus some data even being younger than the age of the stratigraphic cover. The presence of andesite dikes and of pebbles and cobbles (< 20 cm) of basalt, andesite, rhyolite and of rhyolitic tuff in the Triassic carbonate platform deposits indicates that within the Transdanubian Range formed a volcanic complex in Triassic. The major mineralogical and geochemical features of the Transdanubian igneous suite are similar to the Triassic formations in the Southern Alps. However, dissimilar zircon composition excludes the immediate relationship of the zircon-bearing silicic formations in the two tectonic units. New U–Pb ages show that the beginning of the volcanic activity is probably coeval with the eruption of the widespread “pietra verde” trachytic tuffs in the Upper Anisian–Ladinian successions, but the majority of the ages are younger than those ash layers. The new age constraints give a bench-mark for the termination of the volcanic activity in Carnian time in the Transdanubian Range."],["dc.identifier.doi","10.1007/s00531-019-01714-w"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/16152"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/59971"],["dc.language.iso","en"],["dc.notes.intern","Merged from goescholar"],["dc.relation.issn","1437-3262"],["dc.rights","CC BY 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0"],["dc.subject.ddc","550"],["dc.title","Traces of Carnian volcanic activity in the Transdanubian Range, Hungary"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","390"],["dc.bibliographiccitation.issue","11"],["dc.bibliographiccitation.journal","Geosciences"],["dc.bibliographiccitation.volume","8"],["dc.contributor.author","Sirevaag, Hallgeir"],["dc.contributor.author","Jacobs, Joachim"],["dc.contributor.author","Dunkl, István"],["dc.contributor.author","Läufer, Andreas"],["dc.contributor.author","Ksienzyk, Anna K."],["dc.date.accessioned","2020-12-10T18:47:06Z"],["dc.date.available","2020-12-10T18:47:06Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.3390/geosciences8110390"],["dc.identifier.eissn","2076-3263"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/78647"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.publisher","MDPI"],["dc.relation.eissn","2076-3263"],["dc.rights","https://creativecommons.org/licenses/by/4.0/"],["dc.title","Tectono-Thermal Evolution and Morphodynamics of the Central Dronning Maud Land Mountains, East Antarctica, Based on New Thermochronological Data"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","640"],["dc.bibliographiccitation.issue","6"],["dc.bibliographiccitation.journal","Minerals"],["dc.bibliographiccitation.volume","11"],["dc.contributor.author","Molnár, Zsuzsa"],["dc.contributor.author","Kiss, Gabriella B."],["dc.contributor.author","Molnár, Ferenc"],["dc.contributor.author","Váczi, Tamás"],["dc.contributor.author","Czuppon, György"],["dc.contributor.author","Dunkl, István"],["dc.contributor.author","Zaccarini, Federica"],["dc.contributor.author","Dódony, István"],["dc.date.accessioned","2021-08-12T07:46:02Z"],["dc.date.available","2021-08-12T07:46:02Z"],["dc.date.issued","2021"],["dc.description.abstract","The middle Anisian extensional tectonics of the Neotethyan realm developed a small, isolated carbonate platform in the middle part of the Balaton Highland (western Hungary), resulted in the deposition of uranium-bearing seamount phosphorite on the top of the drowned platform and produced some epigenetic fluorite veins in the Middle Triassic sequence. The stable C-O isotope data of carbonates are shifted from the typical Triassic carbonate ranges, confirming the epigenetic-hydrothermal origin of veining. Primary fluid inclusions in fluorite indicate that these veins were formed from low temperature (85–169 °C) and high salinity NaCl + CaCl2 + H2O type (apparent total salinity: 15.91–22.46 NaCl wt%) hydrothermal fluids, similar to parent fluids of the Alpine-type Pb-Zn deposits. These findings indicate that the Triassic regional fluid circulation systems in the Alpine platform carbonates also affected the area of the Balaton Highland. This is also in agreement with the previously established palinspatic tectonic reconstructions indicating that the Triassic carbonate and basement units in the Balaton Highland area were a part of the Southern Alpine. Similar fluorite veining in phosphorite deposits is also known in the Southern Alpine areas (e.g., Monte San Giorgi, Italy). Raman spectroscopic analyses detected H2 gas in the vapor phase of the fluid inclusions and a defect-rich fluorite structure in violet to black colored growth zones. This unique phenomenon is assumed to be the result of interaction between the uranium-rich phosphorite and the parent fluids of the epigenetic fluorite veins."],["dc.description.abstract","The middle Anisian extensional tectonics of the Neotethyan realm developed a small, isolated carbonate platform in the middle part of the Balaton Highland (western Hungary), resulted in the deposition of uranium-bearing seamount phosphorite on the top of the drowned platform and produced some epigenetic fluorite veins in the Middle Triassic sequence. The stable C-O isotope data of carbonates are shifted from the typical Triassic carbonate ranges, confirming the epigenetic-hydrothermal origin of veining. Primary fluid inclusions in fluorite indicate that these veins were formed from low temperature (85–169 °C) and high salinity NaCl + CaCl2 + H2O type (apparent total salinity: 15.91–22.46 NaCl wt%) hydrothermal fluids, similar to parent fluids of the Alpine-type Pb-Zn deposits. These findings indicate that the Triassic regional fluid circulation systems in the Alpine platform carbonates also affected the area of the Balaton Highland. This is also in agreement with the previously established palinspatic tectonic reconstructions indicating that the Triassic carbonate and basement units in the Balaton Highland area were a part of the Southern Alpine. Similar fluorite veining in phosphorite deposits is also known in the Southern Alpine areas (e.g., Monte San Giorgi, Italy). Raman spectroscopic analyses detected H2 gas in the vapor phase of the fluid inclusions and a defect-rich fluorite structure in violet to black colored growth zones. This unique phenomenon is assumed to be the result of interaction between the uranium-rich phosphorite and the parent fluids of the epigenetic fluorite veins."],["dc.description.sponsorship","European Union’s Horizon 2020 research and innovation program"],["dc.identifier.doi","10.3390/min11060640"],["dc.identifier.pii","min11060640"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/88602"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-448"],["dc.publisher","MDPI"],["dc.relation.eissn","2075-163X"],["dc.rights","https://creativecommons.org/licenses/by/4.0/"],["dc.title","Epigenetic-Hydrothermal Fluorite Veins in a Phosphorite Deposit from Balaton Highland (Pannonian Basin, Hungary): Signatures of a Regional Fluid Flow System in an Alpine Triassic Platform"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]