SUMMARY: The crystallographic orientations of calcite in tectonites from the Morcles Nappe and the Glarus Overthrust have been measured by X-ray texture goniometry. The orientation data are represented bypole figures, inverse pole figures and as orientation distribution functions. The patterns of preferred orientation ~observed in the specimens from the Morcles Nappe are correlated with intracrystalline slip mechanisms. The patterns exhibit quasi-axial symmetry and in some cases the axis of symmetry isoblique to the symmetry of the macroscopic fabric. This obliquity is interpreted as the result of a rotational strain path and may be used to infer direction and sense of shear. Some specimens of the Lochseiten mylonite from the Glarus Thrust ...
Samples of fault gouge from the San Andreas Fault drill hole (SAFOD), a shale from the North Sea sed...
A sample of anorthosite from the granulite facies Morin Shear Zone (Quebec, Canada) was investigated...
The Gressoney Shear Zone (GSZ) consists of a ca. 500 m thick, intensely deformed rock panel located ...
The microstructural and quantitative texture analyses of a naturally deformed calcite mylonite, a do...
The correct determination of the kinematic rotation axis (vorticity) in high-strain zones is essenti...
The quartz microstructures and microfabrics in tectonites representing greenschist to granulite faci...
The experiments described are a continuation of a series of tests on Solnhofen limestone, Carrara ma...
Crystal preferred orientation of 47 samples of quartzite and eight samples of associated marbles fro...
Folds with hinge lines subparallel to stretching lineation are common features in shear zones and re...
Microstructures and textures of calcite mylonites from the Morcles nappe large-scale shear zone in s...
In the geologic record, the quartz c-axis patterns are widely adopted in the investigation of crysta...
Limestone from the Hampton Formation at Ferguson, Iowa, was studied in an effort to determine whethe...
Grain size reduction due to cataclasis is a key process controlling fault frictional properties duri...
The orientation of the Valleys in Switzerland shows a remarkable symmetry. It is the aim of this pap...
Crystals orientation in polycrystalline natural compounds maybe either completely random or else fol...
Samples of fault gouge from the San Andreas Fault drill hole (SAFOD), a shale from the North Sea sed...
A sample of anorthosite from the granulite facies Morin Shear Zone (Quebec, Canada) was investigated...
The Gressoney Shear Zone (GSZ) consists of a ca. 500 m thick, intensely deformed rock panel located ...
The microstructural and quantitative texture analyses of a naturally deformed calcite mylonite, a do...
The correct determination of the kinematic rotation axis (vorticity) in high-strain zones is essenti...
The quartz microstructures and microfabrics in tectonites representing greenschist to granulite faci...
The experiments described are a continuation of a series of tests on Solnhofen limestone, Carrara ma...
Crystal preferred orientation of 47 samples of quartzite and eight samples of associated marbles fro...
Folds with hinge lines subparallel to stretching lineation are common features in shear zones and re...
Microstructures and textures of calcite mylonites from the Morcles nappe large-scale shear zone in s...
In the geologic record, the quartz c-axis patterns are widely adopted in the investigation of crysta...
Limestone from the Hampton Formation at Ferguson, Iowa, was studied in an effort to determine whethe...
Grain size reduction due to cataclasis is a key process controlling fault frictional properties duri...
The orientation of the Valleys in Switzerland shows a remarkable symmetry. It is the aim of this pap...
Crystals orientation in polycrystalline natural compounds maybe either completely random or else fol...
Samples of fault gouge from the San Andreas Fault drill hole (SAFOD), a shale from the North Sea sed...
A sample of anorthosite from the granulite facies Morin Shear Zone (Quebec, Canada) was investigated...
The Gressoney Shear Zone (GSZ) consists of a ca. 500 m thick, intensely deformed rock panel located ...