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Record W4408488003 · doi:10.5194/egusphere-egu25-9894

Detachment versus strike-slip ductile shearing in the Nordrahmen Zone of the Tauern Window

2025· preprint· en· W4408488003 on OpenAlex
Bernhard Grasemann, Benjamin Huet, David Schneider, Gerd Rantitsch, Wolfgang Frank

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

affAt least one author lists a Canadian institution in the pinned OpenAlex snapshot.

Bibliographic record

Venuenot available
Typepreprint
Languageen
FieldEngineering
TopicCivil and Structural Engineering Research
Canadian institutionsUniversity of Ottawa
Fundersnot available
KeywordsShearing (physics)GeologyWindow (computing)Slip (aerodynamics)SeismologyGeotechnical engineeringComputer scienceEngineeringOperating system

Abstract

fetched live from OpenAlex

The Tauern Window in the Eastern Alps (Austria) is one of the most prominent tectonic windows, which exposes Subpenninic and Penninic nappes derived from the European margin and Alpine Tethys respectively below the Austroalpine Unit derived from the Adriatic continent. Along the northeastern margin of the window, in the so-called Nordrahmen Zone (NRZ), subvertical W-E striking marble mylonites, graphitic schists and phyllonites with a subhorizontal stretching lineation record intense ductile shear deformation. Previous studies suggested that these structures record the ductile history of a major sinistral strike-slip fault (i.e. the Salzach-Ennstal-Mariazell-Puchberg Fault System), which accommodated the Miocene lateral extrusion of the central parts of the Eastern Alps towards the Pannonian Basin.In this work, we investigated a N-S section along the Grossarl valley, which demonstrates that the subvertical mylonitic rocks are deformed into upright folds with wavelengths and amplitudes on the order of several hundreds of meters and fold axes that are parallel to the mylonitic W-E trending stretching lineation. Reversal of the apparent strike-slip shear sense in the fold limbs suggests that the mylonites have been folded after shear deformation and that mylonites record top-E shearing when unfolded. Ductile subvertical flattening is recorded by a second fold generation with similar W-E trending fold axis but subhorizontal axial planes forming Type 3 refold structures. Ductile top-E shearing is documented by low-angle E-dipping ductile shear zones, shear bands, SC and SCC’ fabrics and brittle ductile conjugate N-S striking high-angle faults. Shear deformation intensifies towards higher structural levels localizing in ultramylonites and cellular dolomite cataclasites below almost undeformed klippen of quartzites and dolomites (Mt. Schuhflicker and Mt. Saukarkopf), which belong to the Lower Austroalpine Unit. Using Raman Spectroscopy of Carbonaceous Materials, we constrain the temperature of mylonitization between 350°C and 400°C. Comparison with published Ar/Ar ages from the Nordrahmen Zone suggests that mylonitization operated around 30 Ma.We therefore suggest that the mylonites along the northeastern margin of the Tauern Window are not part of a strike-slip fault system. They actually belong to a major top-E detachment system, which records an early stage of the exhumation of the Tauern Window before deformation localized along the Miocene Katschberg Normal Fault at the eastern margin of the Tauern Window.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Simulation or modeling · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.498
Threshold uncertainty score0.658

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0010.001
Research integrity0.0000.001
Insufficient payload (model declined to judge)0.0000.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.018
GPT teacher head0.258
Teacher spread0.239 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it