Zobrazeno 1 - 10 of 60 pro vyhledávání: '"Bernhard Fügenschuh"'
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First results of zoned garnet Lu-Hf geochronology in micaschists from the Eoalpine high-pressure-belt, Eastern Alps
Autor: Kathrin Fassmer, Peter Tropper, Hannah Pomella, Christoph Hauzenberger, Carsten Münker, Bernhard Fügenschuh
In collisional orogens continental crust is subducted to (ultra-)high-pressure (HP/UHP) conditions as constrained by petrologic, tectonic and geophysical observations. Despite a wealth of studies on the subduction and exhumation of UHP rocks, the dur
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::00c172551ac43b2f271c019fab93abf9
https://doi.org/10.5194/egusphere-egu22-7476
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5
Internal deformation of the Dolomites Indenter, eastern Southern Alps: An integrated field, thermochronology and physical analogue modelling approach
Autor: Hannah Pomella, Bernhard Fügenschuh, Anna-Katharina Sieberer, Hugo Ortner, Ernst Willingshofer, Thomas Klotz
The Dolomites Indenter (DI) represents the front of the Neogene to ongoing N(W)-directed continental indentation of Adria into Europe. Deformation of the DI is well studied along its rim, documented by important fault zones as, e.g., the Periadriatic
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::aa331c67c25703acd03470b2adf43d68
https://doi.org/10.5194/egusphere-egu21-13598
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7
Post-Variscan metamorphism in the Apuseni and Rodna Mountains (Romania): evidence from Sm–Nd garnet and U–Th–Pb monazite dating
Autor: Elena Negulescu, Bernhard Fügenschuh, Martin Reiser, Ralf Schuster, Gavril Săbău, Peter Tropper
Publikováno v: Swiss Journal of Geosciences. 112:101-120
The Tisza and Dacia mega-units constitute a central part of the Alps-Carpathians-Dinarides orogenic system. Polyphase medium-grade metamorphism observed in mineral assemblages from the crystalline basement is often correlated with Variscan and pre-Va
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::9b00d60dc0806b434cc8ccca5c5d56fc
https://doi.org/10.1007/s00015-018-0322-7
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8
Constraints on the depositional age and tectonometamorphic evolution of marbles from the Biharia Nappe System (Apuseni Mountains, Romania)
Autor: Peter Tropper, Ralf Schuster, Martin Reiser, Bernhard Fügenschuh
Publikováno v: Geologica Carpathica, Vol 68, Iss 2, Pp 147-166 (2017)
Basement rocks from the Biharia Nappe System in the Apuseni Mountains comprise several dolomite and calcite marble sequences or lenses which experienced deformation and metamorphic overprint during the Alpine orogeny. New Sr, O and C-isotope data in
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9bc1fdfb629c522282d03094b02cb7d5
https://doi.org/10.1515/geoca-2017-0012
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10
From nappe stacking to exhumation: Cretaceous tectonics in the Apuseni Mountains (Romania)
Autor: Bernhard Fügenschuh, Martin Reiser, Peter Tropper, Richard Alan Spikings, Ralf Schuster
Publikováno v: International Journal of Earth Sciences
New Ar–Ar muscovite and Rb–Sr biotite age data in combination with structural analyses from the Apuseni Mountains provide new constraints on the timing and kinematics of deformation during the Cretaceous. Time–temperature paths from the structu
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::40873844f34e6dfc3ae3923fa5789a60
https://doi.org/10.1007/s00531-016-1335-y
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