Dunkl, István

[["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","60"],["dc.bibliographiccitation.journal","Austrian Journal of Earth Sciences"],["dc.bibliographiccitation.lastpage","69"],["dc.bibliographiccitation.volume","101"],["dc.contributor.author","Kuhlemann, Joachim"],["dc.contributor.author","Taubald, Heinrich"],["dc.contributor.author","Vennemann, Torsten"],["dc.contributor.author","Dunkl, Istvan"],["dc.contributor.author","Frisch, Wolfgang"],["dc.date.accessioned","2018-11-07T11:19:28Z"],["dc.date.available","2018-11-07T11:19:28Z"],["dc.date.issued","2008"],["dc.description.abstract","Red clays from Cenozoic palaeosols of the Eastern Alps record periods of stagnating uplift and decrease of relief. Tropical to sub-tropical weathering of a crystalline substratum formed dominant or abundant kaolinite, reflecting Paleogene and Early Miocene conditions, respectively. Abundant illite and chlorite, but a lack of kaolinite in red clays on the plateaus of the Northern Calcareous Alps reflects feldspar-poor compositons of the Cenozoic siliciclastic cover. The presence of high Ba/Sr and Rb/Sr ratios and vermiculite in these red clays indicates high precipitation and temperate weathering conditions, respectively, during the Late Miocene and Early Pilocene on the uplifting plateaus of the Northern Calcareous Alps."],["dc.identifier.isi","000267283400006"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/55288"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Oesterreichische Geologische Gesellschaft"],["dc.relation.issn","2072-7151"],["dc.title","CLAY MINERAL AND GEOCHEMICAL COMPOSITION OF CENOZOIC PALEOSOL IN THE EASTERN ALPS (AUSTRIA)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","S225"],["dc.bibliographiccitation.journal","Swiss Journal of Geosciences"],["dc.bibliographiccitation.lastpage","S233"],["dc.bibliographiccitation.volume","101"],["dc.contributor.author","Danisik, Martin"],["dc.contributor.author","Kohut, Milan"],["dc.contributor.author","Dunkl, Istvan"],["dc.contributor.author","Hrasko, Lubomir"],["dc.contributor.author","Frisch, Wolfgang"],["dc.date.accessioned","2018-11-07T11:20:49Z"],["dc.date.available","2018-11-07T11:20:49Z"],["dc.date.issued","2008"],["dc.description.abstract","The thermal evolution of the only known Alpine (Cretaceous) granite in the Western Carpathians (Rochovce granite) is studied by low-temperature thermochronological methods. Our apatite fission track and apatite (U-Th)/He ages range from 17.5 +/- 1.1 to 12.9 +/- 0.9 Ma, and 12.9 +/- 1.8 to 11.3 +/- 0.8 Ma. respectively. The data thus show that the Rochovce granite records a thermal event in the Middle to early Late Miocene, which was likely related to mantle upwelling, volcanic activity, and increased heat flow. During the thermal maximum between similar to 17 and 8 Ma, the granite was heated to temperatures equal to or greater than 60 degrees C. Increase of cooling rates at similar to 12 Ma recorded by the apatic fission track and (U-Th)/He data is primarily related to the cessation of the heating event and relaxation of the isotherms associated with the termination of the Neogene volcanic activity. This contradicts the accepted concept, which stipulates that the internal parts of the Western Carpathians were not thermally affected during the Cenozoic period. The Miocene thermal event was not restricted to the investigated part of the Western Carpathians, but had regional character and affected several basement areas in the Western Carpathians, the Pannonian basin and the margin of the Eastern Alps."],["dc.description.sponsorship","German Science Foundation"],["dc.identifier.doi","10.1007/s00015-008-1279-8"],["dc.identifier.isi","000263223600013"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/55629"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Springer"],["dc.publisher.place","Basel"],["dc.relation.issn","1661-8734"],["dc.relation.issn","1661-8726"],["dc.title","Apatite fission track and (U-Th)/He thermochronology of the Rochovce granite (Slovakia) - implications for the thermal evolution of the Western Carpathian-Pannonian region"],["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","1-4"],["dc.bibliographiccitation.journal","Tectonophysics"],["dc.bibliographiccitation.lastpage","99"],["dc.bibliographiccitation.volume","504"],["dc.contributor.author","Marton, Emo"],["dc.contributor.author","Zampieri, Dario"],["dc.contributor.author","Kazmer, Miklos"],["dc.contributor.author","Dunkl, Istvan"],["dc.contributor.author","Frisch, Wolfgang"],["dc.date.accessioned","2018-11-07T08:56:14Z"],["dc.date.available","2018-11-07T08:56:14Z"],["dc.date.issued","2011"],["dc.description.abstract","From the \"undeformed\" foreland of the Southern Alps Paleocene through Early Miocene rocks, mostly biostratigraphically well-dated sediments with sub-horizontal bed attitude were collected for a paleomagnetic study from 23 geographically distributed localities. The samples were subjected to standard paleomagnetic measurements and evaluation. While the Miocene samples are unstable, most of the older localities yielded statistically well-defined paleomagnetic directions. These are interpreted as primary for the compact marls, supported by positive between-locality tilt and reversal tests. This large group of localities is characterized by CCW rotated declinations with respect to the present north. Combined with paleomagnetic directions of corresponding age from stable Istria, these allow definition of the APW for stable Adria for the 61.6-33.9 Ma interval, which is significantly displaced from the coeval segment of the African APW due to the decoupling of the former to the latter by a moderate CCW rotation. This post-Eocene final separation (exact age is not constrained directly, but estimated as end-of-Miocene) was preceded by a small CW rotation of Adria with respect to Africa, suggested by unchanged orientation of the former across the Cretaceous Paleocene boundary, while the latter continued its CCW rotation. (C) 2011 Elsevier B.V. All rights reserved."],["dc.identifier.doi","10.1016/j.tecto.2011.03.006"],["dc.identifier.isi","000291296400008"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/23092"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Elsevier Science Bv"],["dc.relation.issn","0040-1951"],["dc.title","New Paleocene-Eocene paleomagnetic results from the foreland of the Southern Alps confirm decoupling of stable Adria from the African plate"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","273"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","Zeitschrift für Geomorphologie"],["dc.bibliographiccitation.lastpage","289"],["dc.bibliographiccitation.volume","52"],["dc.contributor.author","Danisik, Martin"],["dc.contributor.author","Panek, Tomas"],["dc.contributor.author","Matysek, Dalibor"],["dc.contributor.author","Dunkl, Istvan"],["dc.contributor.author","Frisch, Wolfgang"],["dc.date.accessioned","2018-11-07T11:11:58Z"],["dc.date.available","2018-11-07T11:11:58Z"],["dc.date.issued","2008"],["dc.description.abstract","The age of planation surfaces in the Podbeskydska pahorkatina Upland in the Outer Western Carpathians (OWC, Czech Republic) is constrained by low-temperature thermochronological dating methods for the first time. Our apatite fission track and apatite (U-Th)/He data measured on teschenite intrusions show that planation surfaces in the study area formed in post-Pannonian time (> 7.1 Ma) and are therefore younger than traditionally believed. This contradicts the classical concepts, which stipulate that a large regional planation surface of Pannonian age (the so-called \"midmountain level\") developed in the whole Western Carpathians. Geodynamic implications of our data are the following: (i) the investigated Tesin and Godula nappes of the OWC were buried and thermally overprinted in the accretionary wedge in different ways, and consequently experienced different cooling histories. This indicates a dynamic basin setting with an active accretionary process in a subduction zone; (ii) accretionary processes in the OWC were active already during Late Eocene times."],["dc.identifier.doi","10.1127/0372-8854/2008/0052-0273"],["dc.identifier.isi","000259549200001"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/53553"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Gebruder Borntraeger"],["dc.relation.issn","0372-8854"],["dc.title","Apatite fission track and (U-Th)/He dating of teschenite intrusions gives time constraints on accretionary processes and development of planation surfaces in the Outer Western Carpathians"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","S255"],["dc.bibliographiccitation.journal","Swiss Journal of Geosciences"],["dc.bibliographiccitation.lastpage","S271"],["dc.bibliographiccitation.volume","101"],["dc.contributor.author","Fodor, Laszlo I."],["dc.contributor.author","Gerdes, Axel"],["dc.contributor.author","Dunkl, Istvan"],["dc.contributor.author","Koroknai, Balazs"],["dc.contributor.author","Pecskay, Zoltan"],["dc.contributor.author","Trajanova, Mirka"],["dc.contributor.author","Horvath, Peter"],["dc.contributor.author","Vrabec, Marko"],["dc.contributor.author","Jelen, Bogomir"],["dc.contributor.author","Balogh, Kadosa"],["dc.contributor.author","Frisch, Wolfgang"],["dc.date.accessioned","2018-11-07T11:20:49Z"],["dc.date.available","2018-11-07T11:20:49Z"],["dc.date.issued","2008"],["dc.description.abstract","New laser ablation-inductive Coupled plasma-mass Spectrometry U-Pb analyses on oscillatory-zoned zircon imply Early Miocene crystallization (18.64 +/- 0.11 Ma) of the Pohorje pluton at the southeastern margin of the Eastern Alps (northern Slovenia). Inherited zircon cores indicate two crustal sources: I late Variscan magmatic population (similar to 270-290 Ma) and in early Neoproterozoic one (850-900 Ma) With juvenile Hf isotope composition close to that of depleted mantle. Initial epsilon Hf of Miocene zircon points to an additional, more juvenile Source component of the Miocene magma, which could be either a juvenile Phanerozoic crust or the Miocene mantle. The new U-Pb isotope age of the Pohorje pluton seriously questions its attribution to the Oligocene age 'Periadriatic' intrusions. The new data imply a temporal coincidence with 19-15 Ma magmatism in the Pannonian Basin system. more specifically in the Styrian Basin. K-Ar mineral-, and whole rock ages from the pinion itself and cogenetic shallow intrusive dacitic rocks (similar to 18-16 Ma), as well as zircon fission track data (17.7-15.6 Ma), gave late Early to early Middle Miocene ages, indicating rapid cooling of the pluton within about 3 Million years. Medium-grade Austroalpine metamorphics north and South of the pluton were reheated and subsequently cooled together. Outcrop- and micro scale structures record deformation of the Pohorje pluton and few related mafic and dacitic dykes under greenschist facies conditions. Part of the solid-state fabrics indicate E-W oriented stretching and vertical thinning, while steeply dipping foliation and NW-SE trending lineation are also present. The E-W oriented lineation is parallel to the direction of subsequent brittle extension, Which resulted in normal faulting and filling of the earlier ductile fabric at around the Early / Middle Miocene boundary normal faulting was combined with strike-slip faulting. Renewed N-S compression may be related to late Miocene to Quaternary dextral faulting in the area. The documented syn-cooling extensional structures and part of the strike-slip faults can be interpreted as being related to lateral extrusion of the Eastern Alps and/or to back-arc rifting in the Pannonian Basin."],["dc.identifier.doi","10.1007/s00015-008-1286-9"],["dc.identifier.isi","000263223600015"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/55630"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Springer"],["dc.publisher.place","Basel"],["dc.relation.issn","1661-8726"],["dc.title","Miocene emplacement and rapid cooling of the Pohorje pluton at the Alpine-Pannonian-Dinaridic junction, Slovenia"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.artnumber","TC1001"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Tectonics"],["dc.bibliographiccitation.volume","26"],["dc.contributor.author","Danisik, Martin"],["dc.contributor.author","Kuhlemann, Joachim"],["dc.contributor.author","Dunkl, Istvan"],["dc.contributor.author","Szekely, Balazs"],["dc.contributor.author","Frisch, Wolfgang"],["dc.date.accessioned","2018-11-07T11:05:46Z"],["dc.date.available","2018-11-07T11:05:46Z"],["dc.date.issued","2007"],["dc.description.abstract","[ 1] The Mesozoic and Cenozoic exhumation and cooling history of Corsica is reconstructed by fission track ( FT) data on basement and sedimentary rocks. Apatite ages are 105 - 16 Ma; zircon ages are 160-145 Ma. The Jurassic and Cretaceous ages show that parts of the Variscan basement escaped Alpine influence. The basement was thermally affected by rifting prior to Jurassic opening of the Ligurian-Piedmont Ocean; then it cooled to near-surface temperatures. In Paleocene-Eocene times, subduction buried parts of the basement and overlying flysch to greater depth. In the Oligocene, both collapse of the nappe stack and rifting prior to opening of the Ligurian-Provencal Basin affected the apatite FT system of the basement in different, partly overlapping areas causing a complex age pattern. The study shows that thorough analysis of FT data and thermal modeling allow to assign age populations to distinct cooling processes even when several thermotectonic events contributed to generate an intricate age pattern."],["dc.identifier.doi","10.1029/2005TC001938"],["dc.identifier.isi","000243353000001"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/52141"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Amer Geophysical Union"],["dc.relation.issn","0278-7407"],["dc.title","Burial and exhumation of Corsica (France) in the light of fission track data"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","155"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","The Journal of Geology"],["dc.bibliographiccitation.lastpage","173"],["dc.bibliographiccitation.volume","120"],["dc.contributor.author","Danisik, Martin"],["dc.contributor.author","Kuhlemann, Joachim"],["dc.contributor.author","Dunkl, Istvan"],["dc.contributor.author","Evans, Noreen J."],["dc.contributor.author","Szekely, Balazs"],["dc.contributor.author","Frisch, Wolfgang"],["dc.date.accessioned","2018-11-07T09:12:55Z"],["dc.date.available","2018-11-07T09:12:55Z"],["dc.date.issued","2012"],["dc.description.abstract","The age of high-elevation planation surfaces in Corsica is constrained using new apatite (U-Th)/He data, field observations, and published work (zircon fission track, apatite fission track [AFT] data and landform/stratigraphical analysis). Thermal modeling results based on AFT and (U-Th)/He data, and the Eocene sediments uncomformably overlapping the Variscan crystalline basement indicate that present-day elevated planation surfaces in Corsica are the remnants of an erosion surface formed on the basement between similar to 120 and similar to 60 Ma. During the Alpine collision in the Paleocene-Eocene, the Variscan crystalline basement was buried beneath a westward-thinning wedge of flysch, and the eastern portion was overridden by the Alpine nappes. Resetting of the apatite fission track thermochronometer suggests an overburden thickness of >4 km covering Variscan Corsica. Protected by soft sediment, the planation surface was preserved. In the latest Oligocene to Miocene times, the surface was re-exposed and offset by reactivated faults, with individual basement blocks differentially uplifted in several phases to elevations of, in some cases, 12 km. Currently the planation surface remnants occur at different altitudes and with variable tilt. This Corsican example demonstrates that under favorable conditions, paleolandforms typical of tectonically inactive areas can survive in tectonically active settings such as at collisional plate margins. The results of some samples also reveal some discrepancies in thermal histories modeled from combined AFT and (U-Th)/He data. In some cases, models could not find a cooling path that fit both data sets, while in other instances, the modeled cooling paths suggest isothermal holding at temperature levels just below the apatite partial annealing zone followed by final late Neogene cooling. This result appears to be an artifact of the modeling algorithm as it is in conflict with independent geological constraints. Caution should be used when cross-validating the AFT and (U-Th)/He systems both in the case extremely old terrains and in the case of rocks with a relatively simple, young cooling history."],["dc.identifier.doi","10.1086/663873"],["dc.identifier.isi","000301332700003"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/27056"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Univ Chicago Press"],["dc.relation.issn","1537-5269"],["dc.relation.issn","0022-1376"],["dc.title","Survival of Ancient Landforms in a Collisional Setting as Revealed by Combined Fission Track and (U-Th)/He Thermochronometry: A Case Study from Corsica (France)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.issue","15"],["dc.bibliographiccitation.journal","Geochimica et Cosmochimica Acta"],["dc.bibliographiccitation.volume","71"],["dc.contributor.author","Dunkl, Istvan"],["dc.contributor.author","Danisik, Martin"],["dc.contributor.author","Picotti, Vincenzo"],["dc.contributor.author","Frisch, Wolfgang"],["dc.contributor.author","von Eynatten, Hilmar"],["dc.contributor.author","Castellarin, Alberto"],["dc.date.accessioned","2018-11-07T10:59:58Z"],["dc.date.available","2018-11-07T10:59:58Z"],["dc.date.issued","2007"],["dc.format.extent","A243"],["dc.identifier.isi","000248789900498"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/50822"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Pergamon-elsevier Science Ltd"],["dc.publisher.place","Oxford"],["dc.relation.conference","17th Annual V M Goldschmidt Conference"],["dc.relation.eventlocation","Cologne, GERMANY"],["dc.relation.issn","0016-7037"],["dc.title","(U-Th)/He dating of faulting in the Southern Alps"],["dc.type","conference_abstract"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","378"],["dc.bibliographiccitation.issue","5"],["dc.bibliographiccitation.journal","Terra Nova"],["dc.bibliographiccitation.lastpage","384"],["dc.bibliographiccitation.volume","20"],["dc.contributor.author","Woelfler, Andreas"],["dc.contributor.author","Dekant, Christian"],["dc.contributor.author","Danisik, Martin"],["dc.contributor.author","Kurz, Werner A."],["dc.contributor.author","Dunkl, Istvan"],["dc.contributor.author","Putis, Marian"],["dc.contributor.author","Frisch, Wolfgang"],["dc.date.accessioned","2018-11-07T11:10:51Z"],["dc.date.available","2018-11-07T11:10:51Z"],["dc.date.issued","2008"],["dc.description.abstract","Thermal history modelling based on zircon- and apatite fission track and apatite (U-Th)/He data constrain and refine the near-surface exhumation of the south-eastern Tauern Window (Penninic units) and neighbouring Austroalpine basement units in the Eastern Alps. Fast exhumation on both sides of the Penninic/Austroalpine boundary coincides with a period of lateral extrusion and tectonic denudation of the Penninic units in Miocene time (22-12 Ma). The jump to older ages occurs within the Austroalpine unit along the Polinik fault, which therefore defines the boundary between the tectonically denuded units and the hangingwall at that time. According to the different (U-Th)/He ages between the Penninic Hochalm- and Sonnblick Domes we demonstrate a differential cooling history of these two domes in the latest Miocene and early Pliocene."],["dc.identifier.doi","10.1111/j.1365-3121.2008.00831.x"],["dc.identifier.isi","000259411900007"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/53300"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Blackwell Publishing"],["dc.relation.issn","0954-4879"],["dc.title","Late stage differential exhumation of crustal blocks in the central Eastern Alps: evidence from fission track and (U-Th)/He thermochronology"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]