Jan Pleuger
YOU?
Author Swipe
View article: Coupling Phase Equilibrium Modelling and Apatite‐in‐Garnet Elastic Barometry to Unravel the P–T Path of the Micaschist Unit From the Zicavo Metamorphic Complex (Corsica, France)
Coupling Phase Equilibrium Modelling and Apatite‐in‐Garnet Elastic Barometry to Unravel the P–T Path of the Micaschist Unit From the Zicavo Metamorphic Complex (Corsica, France) Open
To gain insights into the pressure–temperature evolution of a scarcely studied portion of the Variscan basement of Corsica in southern Europe, we combined phase equilibrium modelling, Zr‐in‐rutile thermometry and apatite‐in‐garnet elastic …
View article: Pulsed fluid release from subducting slabs caused by a scale-invariant dehydration process
Pulsed fluid release from subducting slabs caused by a scale-invariant dehydration process Open
The chemical composition of a rock has a first-order effect on the onset and duration of rock dehydration. We present a multiscale dataset of chemical heterogeneities found in a low-temperature serpentinite from the Mirdita ophiolite in Al…
View article: New petrological and geochronological results from the Koralpe-Saualpe-Pohorje Complex (Eastern Alps)
New petrological and geochronological results from the Koralpe-Saualpe-Pohorje Complex (Eastern Alps) Open
The Koralpe-Saualpe-Pohorje Complex (KSPC) in the Eastern Alps stretches from SE Austria to NE Slovenia and hosts the type locality for eclogite. Although the KSPC has been studied for decades, some aspects of its tectonometamorphic evolut…
View article: Investigating the Eastern Alpine–Dinaric transition with teleseismic receiver functions: Evidence for subducted European Crust
Investigating the Eastern Alpine–Dinaric transition with teleseismic receiver functions: Evidence for subducted European Crust Open
The tectonic structure of the Eastern Alps is heavily debated with successive geophysical studies unable to resolve areas of ambiguity (e.g., the presence of a switch in subduction polarity and differing crustal models).Here we produce a h…
View article: Peak pressure estimates of Koralpe-Saualpe-Pohorje Complex based on Raman Spectroscopy
Peak pressure estimates of Koralpe-Saualpe-Pohorje Complex based on Raman Spectroscopy Open
<p>The Koralpe-Saualpe-Pohorje Complex in the Eastern Alps represents a lithologically heterogenous (U)HP nappe with eclogite lenses embedded in gneissic and metasedimentary rocks. The aim of this project is to determine whether or n…
View article: Barometric studies on different rock types from the Adula Nappe (Central Alps) by Raman spectroscopy of quartz inclusions in garnet
Barometric studies on different rock types from the Adula Nappe (Central Alps) by Raman spectroscopy of quartz inclusions in garnet Open
<p>The Adula nappe in the Swiss-Italian Central Alps is a continental basement nappe from the former European margin that was subducted to depths indicating (ultra)-high-pressure conditions. Many studies were performed to understand …
View article: Establishing the eastern alpine-dinaric transition with teleseismic receiver functions: Evidence for subducted European Crust
Establishing the eastern alpine-dinaric transition with teleseismic receiver functions: Evidence for subducted European Crust Open
<p>The dense SWATH-D seismic network in the Central-Eastern Alps gives an unprecedented window into the collision of the Adriatic and European plates. We apply the receiver function method to the SWATH-D stations, covering approximat…
View article: Chronometry of a nappe-scale thermal event inferred by thermobarometry and viscous relaxation of quartz inclusion pressure (Adula nappe, Alps)
Chronometry of a nappe-scale thermal event inferred by thermobarometry and viscous relaxation of quartz inclusion pressure (Adula nappe, Alps) Open
<p>The Adula nappe is located at the eastern flank of the Lepontine dome in the Swiss Alps. It consists mainly of orthogneiss and paragneiss with intercalated lenses of eclogite, amphibolite and metasediments. Previous petrological s…
View article: Faulting, doming and basin formation during orogenic arcuation &#8211; the case of the Shkoder-Peja Normal Fault System (northern Albania and Kosovo)
Faulting, doming and basin formation during orogenic arcuation – the case of the Shkoder-Peja Normal Fault System (northern Albania and Kosovo) Open
<p>The junction between the Dinarides and the Hellenides coincides with an orogenic bend characterized by a complex system of faults, domes and sedimentary basins. The major structure at this junction is the Shkoder-Peja Normal Fault…
View article: Filling the Moho gap: High resolution crustal structure of the Eastern Alps
Filling the Moho gap: High resolution crustal structure of the Eastern Alps Open
<p>The dense SWATH-D seismic network in the Central-Eastern Alps gives an unprecedented window into the collision of the Adriatic and European plates. Previous studies have suggested a Moho gap overlying a subduction polarity switch.…
View article: Evolving temperature field in a fossil subduction channel during the transition from subduction to collision (Tauern Window, Eastern Alps)
Evolving temperature field in a fossil subduction channel during the transition from subduction to collision (Tauern Window, Eastern Alps) Open
We investigate the evolution of the three‐dimensional thermal structure of a palaeo‐subduction channel exposed in the Penninic units of the central Tauern Window (Eastern Alps). Structural and petrological observations reveal a sheath fold…
View article: No polarity switch? Continental subduction of European crust below the Eastern Alps imaged by receiver functions
No polarity switch? Continental subduction of European crust below the Eastern Alps imaged by receiver functions Open
<p>In the Eastern Alps, teleseismic tomography suggests that there is a switch from European subduction in the west to Adriatic subduction in the east. The dense SWATH-D seismic network is located in the central-eastern Alps between …
View article: Three-dimensional temperature variations in a fossil subduction zone resolved by RSCM thermometry (Tauern Window, Eastern Alps)
Three-dimensional temperature variations in a fossil subduction zone resolved by RSCM thermometry (Tauern Window, Eastern Alps) Open
<p>Knowledge on the thermal state of orogens and subduction zones is crucial in trying to understand the processes that take place in these zones, since temperature controls, e.g., rock strength, metamorphic reactions and fluid flow.…
View article: The Neotethys suture in the eastern Bulgarian Rhodopes
The Neotethys suture in the eastern Bulgarian Rhodopes Open
<p>Following a tectonic scheme proposed by Jan&#225;k et al. (2011; Journal of Metamorphic Geology 29, 317-332) and Pleuger et al. (2011; Zeitschrift der Deutschen Gesellschaft f&#252;r Geowissenschaften 162, 171-192), the Rh…
View article: Crustal‐Scale Sheath Folding at HP Conditions in an Exhumed Alpine Subduction Zone (Tauern Window, Eastern Alps)
Crustal‐Scale Sheath Folding at HP Conditions in an Exhumed Alpine Subduction Zone (Tauern Window, Eastern Alps) Open
We investigate a well‐preserved paleo subduction channel that preserves a coherent part of the European continental margin exposed in the central Tauern Window (Eastern Alps), with the aim of testing models of sheath fold nappe formation a…
View article: Crustal‐scale sheath folding at HP conditions in an exhumed alpine subduction zone (Tauern Window, Eastern Alps)
Crustal‐scale sheath folding at HP conditions in an exhumed alpine subduction zone (Tauern Window, Eastern Alps) Open
We investigate a well‐preserved paleo subduction channel that preserves a coherent part of the European continental margin exposed in the central Tauern Window (Eastern Alps), with the aim of testing models of sheath fold nappe formation a…
View article: &amp;#8220;Cenozoic deformation in the Tauern Window (Eastern Alps, Austria) constrained by in-situ Th-Pb dating of fissure monazite&amp;#8221; by E. Ricchi et al.
&#8220;Cenozoic deformation in the Tauern Window (Eastern Alps, Austria) constrained by in-situ Th-Pb dating of fissure monazite&#8221; by E. Ricchi et al. Open
The manuscript "Cenozoic deformation in the Tauern Window (Eastern Alps, Austria) constrained by in-situ Th-Pb dating of fissure monazite" by E. Ricchi et al. contains a rather large number of new data that add to extensive thermochronolog…
View article: Coupled Crust‐Mantle Response to Slab Tearing, Bending, and Rollback Along the Dinaride‐Hellenide Orogen
Coupled Crust‐Mantle Response to Slab Tearing, Bending, and Rollback Along the Dinaride‐Hellenide Orogen Open
We integrate structural, geophysical, and geodetic studies showing that the Dinarides‐Hellenides orogen along the Adria‐Europe plate boundary in the Western Balkan peninsula has experienced clockwise oroclinal bending since Eocene‐Oligocen…
View article: Current challenges for explaining (ultra)high‐pressure tectonism in the Pennine domain of the Central and Western Alps
Current challenges for explaining (ultra)high‐pressure tectonism in the Pennine domain of the Central and Western Alps Open
The Pennine domain of the Central and Western ( PCW ) Alps, including the Dora‐Maira, Monte Rosa, Gran Paradiso, Adula/Cima Lunga nappes and the Zermatt‐Saas zone underwent ultrahigh‐ or high‐pressure [(U) HP >1.5 GP a] metamorphism during…
View article: The exhumation of the (U)HP rocks of the Central and Western Penninic Alps: comparison study between thermo-mechanical models and field data
The exhumation of the (U)HP rocks of the Central and Western Penninic Alps: comparison study between thermo-mechanical models and field data Open
The Central and Western Penninic (CWP) Alps form an orogenic wedge of imbricate tectonic nappes. Orogenic wedges form typically at depths < 60 km. Nevertheless, a few nappes and massifs (i.e. Adula/Cima Lunga, Dora-Maira, Monte Rosa, Gran …