Titlebook: Experimental and Natural Rock Deformation / Experimentelle und natürliche Gesteinsverformung; Proceedings of the I Peter Paulitsch Conferen

清洗

https://doi.org/10.1007/978-1-349-14240-8model for intragranular gliding possesses the main [010] maximum, but lacks girdles of [100] and [001]. Hence syntectonic recrystallization, probably accompanied by some intragranular rotation, seems to have been the main orienting mechanism. No speculations are warranted as to the role of annealing

Bronchial-Tubes

Globalization of Services: Friend or Foe? be preserved during deformation and is superimposed by the axial symmetry of the new fabric. A theoretical derivation of the end position has been illustrated after the method of Taylor. The only result of the calculations was that [111] cannot be an end position..Comparison of the stress-strain cu

endocardium

Marc Lipsitch,Mauricio Santillanarature and low strain-rate, orthorhombic strain due to temperature gradients produces “crossed girdles” of c-axes intersecting normal to σ.. An extended specimen shows c-axes concentrated at high angles to the extension direction, σ...In the ß-quartz field, recrystallization during compression yield

sperse

The Chickens Have Come Home to Roost,ception, An.. 010 slip and concomitant kinking occur in the more sodic representatives, and irrational deformation lamellae occur in An.-An.. The latter are planar discontinuities in positions of high resolved shear stress and have strong preferred orientation with reference to the crystallographic

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intolerance

Global Challenges for Identity Policiessively of quartz displaying different girdle patterns of extraordinarily high sharpness, using the A.V.A. technique, showed a clear correlation between the type of the orientation of the quartz, the symmetry in the distribution of the disclosed s-surfaces and the shapes of the quartz grains. A trial

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Conference proceedings 1970ay and experimental structural petrology. The Symposium of the Working Group on X-Ray and Experimental Structural Petrology, held at the invitation of the Deutsche Forschungsgemeinschaft on 17 and 18 February, 1969, in the Mineralogy Institute of the Technische Hochschule Darmstadt, was intended to

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Global Cash Management in Europewas therefore a natural consequence that Sander, already in the early stages of petrofabric analysis, drew special attention to the possibilities of X-ray fabric analysis for the investigation of the smallest fabric units (Sander & Sachs 1930). These methods were later developed by Neff (1956), v. Gehlen (1960), Wenk (1965), and others.

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n and steep s-surfaces. In the adjoining northern areas with progressive minor compression and more gentle s-surface they loose their importance and eventually disappear. Then only the regional gentle B-axes are observed..This example shows the origin of a syntectonic steep B-axial fabric in regions with generally gentle B-axes.