Dunkl, István

[["dc.bibliographiccitation.firstpage","270"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","Terra Nova"],["dc.bibliographiccitation.lastpage","278"],["dc.bibliographiccitation.volume","30"],["dc.contributor.author","Botor, Dariusz"],["dc.contributor.author","Anczkiewicz, Aneta A."],["dc.contributor.author","Dunkl, István"],["dc.contributor.author","Golonka, Jan"],["dc.contributor.author","Paszkowski, Mariusz"],["dc.contributor.author","Mazur, Stanisław"],["dc.date.accessioned","2020-12-10T18:36:30Z"],["dc.date.available","2020-12-10T18:36:30Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.1111/ter.12336"],["dc.identifier.issn","0954-4879"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/76645"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Tectonothermal history of the Holy Cross Mountains (Poland) in the light of low-temperature thermochronology"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","125667"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","Geochemistry"],["dc.bibliographiccitation.volume","80"],["dc.contributor.author","Şengün, Fırat"],["dc.contributor.author","Zack, Thomas"],["dc.contributor.author","Dunkl, István"],["dc.date.accessioned","2021-04-14T08:30:03Z"],["dc.date.available","2021-04-14T08:30:03Z"],["dc.date.issued","2020"],["dc.identifier.doi","10.1016/j.chemer.2020.125667"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/83083"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-399"],["dc.relation.issn","0009-2819"],["dc.title","Provenance of detrital rutiles from the Jurassic sandstones in the Central Sakarya Zone, NW Turkey: U-Pb ages and trace element geochemistry"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","S147"],["dc.bibliographiccitation.issue","S1"],["dc.bibliographiccitation.journal","Mineralogical Magazine"],["dc.bibliographiccitation.lastpage","S171"],["dc.bibliographiccitation.volume","82"],["dc.contributor.author","Molnár, Zsuzsa"],["dc.contributor.author","Kiss, Gabriella B."],["dc.contributor.author","Dunkl, István"],["dc.contributor.author","Czuppon, György"],["dc.contributor.author","Zaccarini, Federica"],["dc.contributor.author","Dódony, István"],["dc.date.accessioned","2020-12-10T18:38:41Z"],["dc.date.available","2020-12-10T18:38:41Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.1180/minmag.2017.081.103"],["dc.identifier.eissn","1471-8022"],["dc.identifier.issn","0026-461X"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/77411"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Geochemical characteristics of Triassic and Cretaceous phosphorite horizons from the Transdanubian Mountain Range (western Hungary): genetic implications"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","8"],["dc.bibliographiccitation.journal","Chemical Geology"],["dc.bibliographiccitation.lastpage","21"],["dc.bibliographiccitation.volume","472"],["dc.contributor.author","Sliwinski, J.T."],["dc.contributor.author","Guillong, M."],["dc.contributor.author","Liebske, C."],["dc.contributor.author","Dunkl, I."],["dc.contributor.author","von Quadt, A."],["dc.contributor.author","Bachmann, O."],["dc.date.accessioned","2020-12-10T14:23:03Z"],["dc.date.available","2020-12-10T14:23:03Z"],["dc.date.issued","2017"],["dc.identifier.doi","10.1016/j.chemgeo.2017.09.014"],["dc.identifier.issn","0009-2541"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/71820"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Improved accuracy of LA-ICP-MS U-Pb ages of Cenozoic zircons by alpha dose correction"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","13333"],["dc.bibliographiccitation.issue","12"],["dc.bibliographiccitation.journal","Journal of Geophysical Research. B, Solid Earth"],["dc.bibliographiccitation.lastpage","13353"],["dc.bibliographiccitation.volume","124"],["dc.contributor.author","Gouiza, M."],["dc.contributor.author","Bertotti, G."],["dc.contributor.author","Charton, R."],["dc.contributor.author","Haimoudane, K."],["dc.contributor.author","Dunkl, I."],["dc.contributor.author","Anczkiewicz, A. A."],["dc.date.accessioned","2020-12-10T18:09:24Z"],["dc.date.available","2020-12-10T18:09:24Z"],["dc.date.issued","2019"],["dc.identifier.doi","10.1029/2019JB017914"],["dc.identifier.eissn","2169-9356"],["dc.identifier.issn","2169-9313"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/73643"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","New Evidence of \\‘Anomalous' Vertical Movements along the Hinterland of the Atlantic NW African Margin"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1823"],["dc.bibliographiccitation.issue","5"],["dc.bibliographiccitation.journal","Solid Earth"],["dc.bibliographiccitation.lastpage","1847"],["dc.bibliographiccitation.volume","11"],["dc.contributor.author","Mock, Samuel"],["dc.contributor.author","von Hagke, Christoph"],["dc.contributor.author","Schlunegger, Fritz"],["dc.contributor.author","Dunkl, István"],["dc.contributor.author","Herwegh, Marco"],["dc.date.accessioned","2021-04-14T08:31:02Z"],["dc.date.available","2021-04-14T08:31:02Z"],["dc.date.issued","2020"],["dc.identifier.doi","10.5194/se-11-1823-2020"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/83459"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-399"],["dc.relation.eissn","1869-9529"],["dc.title","Long-wavelength late-Miocene thrusting in the north Alpine foreland: implications for late orogenic processes"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","78"],["dc.bibliographiccitation.issue","1-2"],["dc.bibliographiccitation.journal","Geomorphology"],["dc.bibliographiccitation.lastpage","89"],["dc.bibliographiccitation.volume","117"],["dc.contributor.author","Danisik, Martin"],["dc.contributor.author","Migon, Piotr"],["dc.contributor.author","Kuhlemann, Joachim"],["dc.contributor.author","Evans, Noreen J."],["dc.contributor.author","Dunkl, Istvan"],["dc.contributor.author","Frisch, Wolfgang"],["dc.date.accessioned","2018-11-07T08:44:03Z"],["dc.date.available","2018-11-07T08:44:03Z"],["dc.date.issued","2010"],["dc.description.abstract","A combination of zircon (U-Th)/He (ZHe), apatite fission track (AFT) and apatite (U-Th-[Sm])/He (AHe) thermochronology is used to constrain the long-term exhumation and erosional history of the Karkonosze Mts. in north-eastern Bohemian Massif by analyzing samples from the highly elevated summit planation surface. ZHe ages from the south-eastern part of the planation surface are 285 +/- 19, 295 +/- 20 and 308 +/- 21 Ma, indicating that the area remained at temperatures below similar to 190 degrees C since the Permian. In contrast, ZHe ages in the western part of the planation surface are mid-Cretaceous, proving that this part was residing at temperatures above similar to 190 degrees C prior to exhumation. The exhumation occurred in the Late Cretaceous, as evidenced by AFT and AHe ages, ranging from 82 +/- 5 to 90 +/- 8 Ma and from 77 +/- 5 to 91 +/- 6 Ma, respectively. Modelled cooling trajectories are characterized by a two-stage cooling history: fast cooling through the apatite partial annealing zone and helium partial retention zone to surface conditions between similar to 90 and similar to 75 Ma, and slow cooling or even thermal stagnation from similar to 75 Ma to present. Although our data do not allow us to resolve the age of the planation surface completely, we narrowed down the number of explanatory options and propose two alternative solutions for the formation of the planation surface: (i) the planation surface represents the remnant of a Permian peneplain, which was buried by Mesozoic sediments of the Central European Basin System and was re-exposed in the Late Cretaceous: or, (ii) the planation surface formed after similar to 75 Ma, after termination of a period of massive erosion documented by thermochronological data and by the sedimentary record in adjacent basins. Cenozoic relief production and uplift of the planation surface, evident from regional landforms and the sedimentary record, is not recorded by thermochronological data. This shows that erosion on the uplifted planation surface since similar to 75 Ma was less than similar to 1.2 km. (C) 2009 Elsevier B.V. All rights reserved."],["dc.description.sponsorship","German Science Foundation"],["dc.identifier.doi","10.1016/j.geomorph.2009.11.010"],["dc.identifier.isi","000276543200006"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/20117"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Elsevier Science Bv"],["dc.relation.issn","0169-555X"],["dc.title","Thermochronological constraints on the long-term erosional history of the Karkonosze Mts., Central Europe"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","89"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","TURKISH JOURNAL OF EARTH SCIENCES"],["dc.bibliographiccitation.lastpage","109"],["dc.bibliographiccitation.volume","27"],["dc.contributor.author","AKDOĞAN, REMZİYE"],["dc.contributor.author","OKAY, ARAL I."],["dc.contributor.author","DUNKL, ISTVÁN"],["dc.date.accessioned","2020-12-10T18:47:39Z"],["dc.date.available","2020-12-10T18:47:39Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.3906/yer-1706-19"],["dc.identifier.eissn","1303-619X"],["dc.identifier.issn","1300-0985"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/78841"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Triassic-Jurassic arc magmatism in the Pontides as revealed by the U-Pb detrital zircon ages in the Jurassic sandstones of northeastern Turkey"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","269"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","TURKISH JOURNAL OF EARTH SCIENCES"],["dc.bibliographiccitation.lastpage","293"],["dc.bibliographiccitation.volume","27"],["dc.contributor.author","ÖZDAMAR, Şenel"],["dc.contributor.author","SUNAL, Gürsel"],["dc.contributor.author","DEMİROĞLU, Muhterem"],["dc.contributor.author","YALTIRAK, Cenk"],["dc.contributor.author","BİLLOR, Mehmet Zeki"],["dc.contributor.author","GEORGIEV, Stoyan"],["dc.contributor.author","HAMES, Willis"],["dc.contributor.author","DUNKL, Istvan"],["dc.contributor.author","AYDIN, Halil Can"],["dc.date.accessioned","2020-12-10T18:47:40Z"],["dc.date.available","2020-12-10T18:47:40Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.3906/yer-1712-14"],["dc.identifier.eissn","1303-619X"],["dc.identifier.issn","1300-0985"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/78842"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Metamorphism, magmatism, and exhumation history of the Tavşanlı Zone, NW Turkey: new petrological constraints"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","177"],["dc.bibliographiccitation.journal","Tectonophysics"],["dc.bibliographiccitation.lastpage","191"],["dc.bibliographiccitation.volume","601"],["dc.contributor.author","Kounov, Alexandre"],["dc.contributor.author","Viola, Giulio"],["dc.contributor.author","Dunkl, Istvan"],["dc.contributor.author","Frimmel, Hartwig E."],["dc.date.accessioned","2018-11-07T09:21:25Z"],["dc.date.available","2018-11-07T09:21:25Z"],["dc.date.issued","2013"],["dc.description.abstract","We propose a refined conceptual model for the Paleo- and Mesozoic morpho-tectonic evolution of the southern African cratonic interior. Constraints are derived from new zircon and apatite fission-track and (U-Th-[Sm)]/He dates (ZFT, AFT, ZHe and AHe) of rocks from the Augrabies Falls and Fish River Canyon regions in South Africa and southern Namibia, respectively. The combined ZFT and ZHe thermochronological results suggest a smooth and simple tectonic evolution, wherein the study area cooled monotonically as one coherent block from the Early Silurian to the Mid Triassic in response to very low denudation rates of less than 5 m/myr. Some of the new zircon ages may indicate a discrete and short-lived period of enhanced cooling interrupting this monotonic cooling during the Mid Devonian-Early Carboniferous. We tentatively correlate this episode to the events that caused the regional hiatus that separates the Cape Supergroup from the overlying Karoo Supergroup. Apatite fission-track and (U-Th-[Sm])/He data joint modeling reveals a period of accelerated regional cooling through 120 to 40 degrees C between 100 and 65 Ma ago. We interpret the latter as most probably due to regional uplift in combination with high river gradients and enhanced erosion rates in the Orange and Fish River basins, which, during the Cretaceous, were probably part of the greater Kalahari River catchment area Based on the apatite results, a denudation rate of ca. 25 m/myr was calculated for the Late Cretaceous. At that time the area was probably characterized by an elevated average altitude and low relief, as indicated by the AFT and AHe age patterns. (C) 2013 Elsevier B.V. All rights reserved."],["dc.identifier.doi","10.1016/j.tecto.2013.05.009"],["dc.identifier.isi","000322944400013"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/29099"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Elsevier Science Bv"],["dc.relation.issn","1879-3266"],["dc.relation.issn","0040-1951"],["dc.title","Southern African perspectives on the long-term morpho-tectonic evolution of cratonic interiors"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]