Structural evolution of intermediate-crustal rocks in a strike-slip and extensional setting (Variscan Odenwald, SW Germany): differential upward transport of metamorphic complexes and changing deformation mechanisms
References (147)
- et al.
Geological interpretation of DEKORP 2-S: A deep seismic reflection profile across the Saxothuringian and possible implications for the Late Variscan structural evolution of Central Europe
Tectonophysics
(1987) - et al.
Deformation mechanisms in a high temperature quartz-feldspar mylonite: evidence for superplastic flow in the lower continental crust
Tectonophysics
(1987) - et al.
Orthogneiss, mylonite and non-coaxial deformation granites: the example of the South Armorican Shear Zone
J. Struct. Geol.
(1979) - et al.
C-slip in quartz from subsolidus deformed granite
Tectonophysics
(1986) - et al.
Deep crustal extensional faulting in the Ivrea Zone of Northern Italy
Tectonophysics
(1987) Quartz shape fabric variation and c-axis fabrics in a ribbon mylonite
J. Struct. Geol.
(1986)- et al.
Flow properties of continental lithosphere
Tectonophysics
(1987) - et al.
Deformation mechanisms in experimentally and naturally deformed amphiboles
Earth Planet. Sci. Lett.
(1975) - et al.
Extensional tectonics, basement uplift and Stephano-Permian collapse basin in a late Varisan metamophic core complex (Montagne Noir, Southern Massif Central
Tectonophysics
(1990) - et al.
Computer models of pressure shadows: a method for strain measurement and shear-sense determination
J. Struct. Geol.
(1987)
A 3-D kinematic model of fabric development in polycrystalline aggregates: comparisons with experimental and natural examples
J. Struct. Geol.
Quartz fabric transition in a cooling syntectonic granite
Tectonophysics
Natural rotated inclusions in non-ideal shear
Tectonophysics
The deformational behaviour of bimineralic limestone-halite aggregates
Tectonophysics
Rock mechanics observations pertinent to the rheology of the continental lithosphere and the localization of strain along shear zones
Tectonophysics
Deformation mechanisms—recognition from natural tectonites
J. Struct. Geol.
Local variations of quartz c-axis orientations in non-coaxial regimes and their significance for the mechanics of S-C fabrics
J. Struct. Geol.
Simple shear deformation and quartz crystallographic fabrics: a possible natural example from the Torridon area of NW Scottland
J. Struct. Geol.
S-C Mylonites
J. Struct. Geol.
The partitioning of deformation in flowing rock masses
Tectonophysics
Plate and intraplate processes of Hercynian Europe during the Late Paleozoic
Tectonophysics
Kinematics of compressional and extensional ductile shearing deformation in a metamorphic core complex of the northeastern Basin and Range
J. Struct. Geol.
Collapse of the thickened Variscan Crust in the French Massif Central, Mont Pilat extensional shear zone and St. Etienne Late Carboniferous basin
Tectonophyics
Tectonics and plate tectonics model for the Variscan belt of Europe
Tectonophysics
Sliding behavior and deformation textures of heated illite gouche
J. Struct. Geol.
The Iapetus model: a plate tectonic concept for the Variscan belt of Europe
Tectonophysics
Stable positions of rigid objects in non-coaxial flow—a study in vorticity analysis
J. Struct. Geol.
Secondary cleavages in ductile shear zones
J. Struct. Geol.
Extensional structures in anisotropic rocks
J. Struct. Geol.
Migration of folding and metamorphism in the Rheinische Schiefergebirge deduced from K-Ar and Rb-Sr age determinations
Strike slip orogen—an explanation for the Hercynides
J. Geol. Soc. London
Petrologische Untersuchungen im Felsberg-Zug (Bergsträsser Odenwald)
Abh. Hess. Landesamt Bodenforsch.
Fabric asymmetry and shear sense in movement zones
Geol. Rundsch.
The role of transiently fine-grained reaction products in syntectonic metamorphism: natural and experimental examples
Can. J. Earth. Sci.
Zur genetischen Deutung der Kinzingite im Schwarzwald und Odenwald
Neues Jahrb. Mineral., Monatsh.
Geologische Untersuchungen im Gebiet des Böllsteiner Odenwaldes
Neues Jahrb. Geol Abh.
Dynamic recrystallization and chemical evolution of clinoamphibole from Senja, Norway
Contrib. Mineral. Petrol.
First results and preliminary interpretation of deep reflection seismic recordings along the profile DEKORP 2S
J. Geophys.
Time-dependent friction and the mechanics of stick-slip
Pure Appl. Geophys.
Modelling of fricton in rocks, I. Experimental results and constitutive equations
J. Geophys. Res.
Effect of humidity on time and velocity dependent friction in rocks
J. Geophys. Res.
Crustalscale thrusting and extension in the Hercynian Schwarzwald and Vosges, Central Europe
Tectonics
Palaeozoic Sedimentation in the northern branch of the mid-European variscides—essay of an interpretation
Provenance and depositional environment of Rhenohercynian synorogenic greywackes from the Giessen Nappe, Germany
Geol. Rundsch.
Tectonostratigraphic units in the Variscan belt of central Europe
Geol. Soc. Am., Spec. Pap.
Synorogenic sedimentation in the Variscan belt of Europe
Bull. Soc. Geol. Fr.
Crustal structure of the Rhenish Massif: results of deep seismic reflection lines DEKORP 2-North and 2-North-Q
Geol. Rundsch.
Mechanical properties of feldspar
Staurolite stability and related parageneses: Theory, experiments and applications
J. Petrol.
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Development of a synorogenic composite sill at deep structural levels of a magmatic arc (Odenwald, Germany). Part 2: Rheological inversion and mullion formation under bulk constriction
2022, Journal of Structural GeologyCitation Excerpt :In all investigated samples, quartz shows two sets of subgrain boundaries, which are aligned parallel to both the prism and the basal planes. These patterns of subgrains, associated with [c]-axes within the foliation plane or near the stretching lineation, have also been described from the central part of Unit III (Krohe, 1992). The ‘chessboard patterns’ reflect prism [c] slip in quartz, which is active at T > 600 °C (Blumenfeld et al., 1986; Mainprice et al., 1986).
Integrated 3D geological modelling of the northern Upper Rhine Graben by joint inversion of gravimetry and magnetic data
2021, TectonophysicsCitation Excerpt :Due to the great lithological similarities, the Spessart is most likely the northeastern extension of the Böllstein Odenwald (Weber, 1995b). The Bergsträßer Odenwald consists mainly of mafic to felsic plutonic rocks, that are intruded into Early Paleozoic metasediments, the so-called ‘Schieferzüge’ (Krohe, 1991, 1992). This unit is again subdivided into the Frankenstein Complex, the Flasergranitoid Zone and the Southern Plutons, each separated by large strike-slip fault zones.