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Rechnitz window group represents a Http://dating.hr-audio.de/handy-flirten-kostenlos.php metamorphic core complex, which is almost entirely located within nearly contemporaneous Neogene sediments at the transition zone between the Eastern Alps and the Neogene Pannonian basin.
Both units are metamorphosed within greenschist single sieggraben conditions during earliest Miocene followed by exhumation and cooling. The internal structure of the RMCC is characterized by the following succession of structure-forming events: E—W to WNW—ESE oriented stretching lineation3 greenschist facies-grade metamorphism annealing dominant in the lower unit, and 4 ductile low-angle normal faulting D 3 with mainly NE—SW oriented stretching lineationand 5 ca.
E to NE-vergent folding D 4. The microfabrics are related to mostly ductile nappe stacking to ductile low-angle normal faulting. Progressive microstructures and texture analysis indicate an overprint of the high-temperature fabrics Partnervermittlung maurer 2 by the low-temperature learn more here D 3.
Chlorite is seemingly accessible to late-stage resetting. The RMCC underwent an earlier large-scale coaxial deformation accommodated by a late non-coaxial shear with ductile low-angle normal faulting, resulting in subvertical thinning in the extensional deformation regime.
The RMCC was rapidly exhumed during ca. Metamorphic core complexes MCCs are particular structures of the continental and oceanic crust within extensional tectonic settings e. Continental core complexes may occur in orogenic settings under an overall regime of plate convergence Whitney et al. Therefore, the middle crustal level position bears important information on the structural and metamorphic evolution of continental crust during continent—continent collision.
Many details single sieggraben article source on the exhumation history and structures single sieggraben to exhumation juxtaposing the typically epidote—amphibolite grade metamorphic MCC to limits ira single roth 2014 income upper plate rocks. However, less attention is paid to the internal structure single sieggraben MCCs and possible overprint structures and microfabrics, which may contribute to the knowledge of intrinsic processes responsible for formation of the MCC structure in a specific geodynamic setting Cao et al.
Due to the strong structural overprint during late-stage or progressive tectonic events, the early single sieggraben history cannot be reconstructed by the investigation of mesoscale structures alone e.
Therefore, macrostructural and microstructural studies combined with the evaluation of lattice-preferred orientation Single sieggraben of main minerals represent important tools for obtaining single sieggraben on deformation mechanisms operating in naturally deformed rocks within such crustal sections.
Here, we describe the structural evolution of a MCC, the greenschist-facies metamorphic Rechnitz window, at the eastern termination of the Eastern Alps, which formed within an extensional single sieggraben and is surrounded by a contemporaneously formed Neogene sedimentary basin Ratschbacher et single sieggraben. However, few detailed investigations of the structure, microstructures and textures have been done within the Rechnitz metamorphic core complex RMCC except for the structure Ratschbacher et al.
This paper presents the evolution of meso- and microstructures, LPOs of quartz and calcite and thermobarometric results of white mica and chlorite from the entire RMCC. These new data constrain the deformational behavior of the RMCC during distinct phases of deformation during polyphase metamorphism. The principal aim of single sieggraben paper is to describe the progressive tectonic evolution of the Penninic units exposed single sieggraben the Rechnitz window, and to trace the history until its exhumation, which makes it to a peculiar Cordilleran-type MCC.
The results have significant implications for the rheological constraints of single sieggraben low-grade MCCs and for the evolution of the Alpine orogen. The Penninic windows are exposed along the central axis of the Eastern Alps, and include the Tauern window and the Rechnitz window Fig.
All of the these windows expose the infill of the Jurassic-Cretaceous Penninic ocean Schmid, and references thereinwhich was subducted underneath continue reading northern Austroalpine margin of the continental Adriatic microplate and which was metamorphosed link high-pressure conditions during Cretaceous or Paleogene times and overprinted by Oligocene to Early Miocene regional metamorphism.
Only the Tauern window exposes the Variscan Central Gneiss basement unit and the overlying Upper Carboniferous to Cretaceous cover, which read article underlying the single sieggraben infill of the Penninic Ocean. The Rechnitz window group represents the easternmost Penninic windows of the Alps and that is single sieggraben one partly covered by Neogene sediments Karpatian in the local Paratethyan time scale: In single sieggraben paper, we only deal with the Rechnitz window, which is the largest of these four windows.
In all Penninic windows, initial stacking of an upper ophiolite unit over lower continent-derived cover units occurred within a subduction channel and units were affected by initial high-pressure metamorphism. Subsequent exhumation of previously subducted and stacked units was accompanied by amphibolite single sieggraben metamorphic conditions in the central Tauern window and by greenschist facies metamorphic single sieggraben in all single sieggraben Penninic windows mentioned above Koller,Koller,Koller and Pahr,Koller and Richter,Kurz et al.
Peak conditions of the regional metamorphic overprint within Penninic windows were likely reached during the Oligocene although data are scarce except for the Tauern window. Oligocene to Miocene single sieggraben was accompanied by ca. Extension also resulted in single sieggraben of both orogenic crust and lithosphere.
The South Burgenland High is a horst structure within the thinned orogenic crust of ca. As mentioned above, exhumation of the Tauern window and the Rechnitz window group is considered as one system, which is partly single sieggraben by brittle extension of single sieggraben hangingwall Single sieggraben unit, which also carries halfgraben-type basins Fig.
The history of research of the Rechnitz window dates back to the nineteenth century and is compiled in PahrRatschbacher et al. The Rechnitz window group mainly exposes various types of phyllites, calcareous phyllites, thin quartzites and marbles, serpentinites, and greenschists. The Rechnitz window has been overthrusted by the Austroalpine nappe complex Fig. The lowest Austroalpine units are represented by the Wechsel and Kirchberg—Stuhleck nappes.
Single sieggraben elsewhere in the Austroalpine nappe complex, these units are overprinted by Cretaceous-age single sieggraben mostly within greenschist-facies conditions in Wechsel and Kirchberg—Stuhleck nappes Dallmeyer et al. The contact between Rechnitz window and the overlying Kirchberg nappe with the Grobgneiss unit is poorly single sieggraben тоже singletrails vogtland быстро the northwestern corner of the Rechnitz window and is more continuous around the Bernstein window Fig.
The Rechnitz window single sieggraben and overlying tectonic units are located along the South Burgenland High e. The tectonostratigraphy of eastern sectors of the Austroalpine units is shown in Fig.
The later contact means that all units from the Wechsel to Sieggraben nappes are cut out by late-stage normal faulting. In summary, the distribution of Austroalpine nappes shows tectonically thinned single sieggraben cut, that we interpret this вот partnervermittlung polen karlsruhe выдалась as the result of semi-ductile to brittle normal faulting.
No later thermal overprint on Austroalpine units subsequent to the above mentioned Late Cretaceous mineral ages was detected by Ar—Ar mineral dating. Zircon single sieggraben ages range from The RMCC is bordered by low-angle normal faults along its eastern and western margins e.
The major faults single sieggraben interpreted to have triggered unroofing and subsequent exhumation of the RMCC.
Representative microfabrics and calcite textures of the western part of the Rechnitz window were published by Ratschbacher et single sieggraben. Zircon FT ages decrease towards the east due to the gradual southward sliding of the overlying Austroalpine nappe complex along low-angle normal faults, suggesting later exhumation in the single sieggraben related to the rolling hinge model. Outcrop-scale structural features, e. All thin single sieggraben prepared for microfabric and texture analysis were cut parallel to the kinematic XZ plane X — parallel to lineation, Y — parallel to foliation and normal to lineation, and Z — normal to foliation.
Mineral deformation features and rock microstructure are characterized with special reference to quartz, feldspar, mica and calcite. Single sieggraben deformation conditions, e. Thin sections were cut from the samples and polished using Buehler Mastermet colloidal silica and the dating detox gemma burgess mobilism Buehler grinder-polisher.
Conducting resin taps attached to the sample surface surrounding the measurement area were used to reduce charging effects. The EBSP data acquisition was done using both point scan and mapping modes.
Indexing was accepted when at least six detected kikuchi bands matched with those in the standard reflector file for the analyzed mineral phases and indexed points with single sieggraben Mean Angular Deviation MAD larger than 1. Although single sieggraben small step sizes will produce duplicate measurements in some big grains, the results are statistically reliable.
The pole figures were plotted in equal area stereographic diagrams of the single sieggraben hemisphere with the trace of the mylonitic foliation Leute regensburg kennenlernen uni and the stretching lineation L as reference directions. Systematic misindexing was noted in automated orientation maps and such data were replaced by zero solution pixels. Natural and synthetic mineral standards were used to calibrate the microprobe and raw data was reduced using standard ZAF correction.
These units have been affected by a polyphase deformation history associated with metamorphism. Our detailed structural analysis reveals that the internal structure of the RMCC is characterized by the following single sieggraben successions of structure-forming events: WSW-dipping axial plane foliation S 4.
Cross-sections as shown in Fig. The scarce blueschists are massive single sieggraben show only a weak foliation and a mineral lineation L 1 composed of fine-grained blue amphibole. No good D 1 structures are preserved in investigated samples and their study single sieggraben outside of the scope of the present study. Mesoscopic deformation D 2 structures are related to ductile nappe stacking developed mostly in the upper nappe and at the top of the lower nappe Figs.
Nappe stacking resulted in the well developed penetrative foliation S 2 and stretching lineation L 2 Fig. The L 2 lineation is generally observed along southern and western sectors of the study area. The foliation and lineation are defined by single sieggraben minerals e. The foliation strikes either N—S west or E—W south and dips moderately single sieggraben to the east, west or south in the schist and phyllite.
The fabrics are largely well annealed due to later heating at greenschist metamorphic conditions. The D single sieggraben deformation stage resulted in dominant pure shear fabrics with article source folds with subhorizontal axial surfaces in the interior of the RMCC observed in the southern part Fig.
Low-temperature D 3 fabrics overprinted simple shear fabrics along попыталась singletreff bad vilbel все-таки see below. Most commonly D 3 deformation is characterized by the development of a second continuous and discontinuous single sieggraben foliation S 3and a ca.
NE-trending stretching lineation L 3 Figs. The lineation is defined by the preferred parallel alignment of the longest dimension of asymmetric feldspar porphyroclasts, stringers of quartz grains, and elongated aggregates of recrystallized quartz and white mica.
D 3 fabrics are tentatively related to ductile low-angle normal faulting, which is related to the formation of the overall RMCC structure. Single sieggraben wide range of kinematic criteria related to D single sieggraben is observed. The different asymmetric fabrics, e. A few S—C fabrics are formed, with Single sieggraben defined by grain aggregates of elongated quartz and feldspar and C-planes single sieggraben chlorite and biotite grains, which also typically show a motion of the hangingwall towards the northeast.
This observation, coupled with penetrative fabrics throughout these rocks recording top-to-the-northeast shearing strain, suggests that the deformation fabrics in rocks resulted from a northeast-directed simple shear.
This check this out interpretation is supported by the microstructural investigations of calcite marble and quartzite outlined as follows below. A common structural feature related to D 4 deformation is the typical mesoscale-style folds along single sieggraben parts of the RMCC.
They are characterized by their axes trend subnormal to L 3 and S single sieggraben D 3 Figs. Single sieggraben 4 is the final stage of ductile upper crustal deformation and does not significantly affect, but bends, the quartz and calcite microfabrics and textures.
Microfabrics and microstructures are mostly related to ductile nappe stacking D 2respectively to ductile low-angle normal faulting D 3. Such characteristics are exemplified by fine-grained mylonitized micaschist, calcite marble and mylonitic phyllite.
Distinctive microstructures were obtained through quartz, feldspar, white single sieggraben and calcite as shown below Fig. Deformed and partly single sieggraben micaschists and single sieggraben are the major constituents of the RMCC, which show well-preserved evidence for two deformation stages Fig.
Quartz microstructures related to D 2 deformation display high-temperature and annealed microfabrics Fig. In the eastern-middle sectors, microstructures developed during D 2 deformation are very well preserved. Sometimes, a preferred orientation of crystallographic axes is missing.
The most common quartz grains show irregular or serrated grain boundaries and single sieggraben subgrain formation, which imply deformation at a relatively single sieggraben temperature by grain boundary migration recrystallization. It is well evidenced single sieggraben during single sieggraben boundary migration white mica is overgrown by dynamically recrystallized quartz grains Fig. The average size of the quartz grains equals ca.
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