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Wiener Geologen im Spiegel des Geologenarchivs.
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- International Journal of Earth Sciences, 2001, v. 90, n. 1, p. 211, doi. 10.1007/s005310000140
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A few remarks on the kinetics of static grain growth in rocks.
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- International Journal of Earth Sciences, 2001, v. 90, n. 1, p. 88, doi. 10.1007/s005310000150
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An evaluation of quartzite flow laws based on comparisons between experimentally and naturally deformed rocks.
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- International Journal of Earth Sciences, 2001, v. 90, n. 1, p. 77, doi. 10.1007/s005310000152
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Fracture process zone in granite: a microstructural analysis.
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- International Journal of Earth Sciences, 2001, v. 90, n. 1, p. 46, doi. 10.1007/s005310000157
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Mechanical twinning of jadeite – an indication of synseismic loading beneath the brittle–plastic transition.
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- International Journal of Earth Sciences, 2001, v. 90, n. 1, p. 4, doi. 10.1007/s005310000165
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Grain size reduction by dynamic recrystallization: can it result in major rheological weakening?
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- International Journal of Earth Sciences, 2001, v. 90, n. 1, p. 28, doi. 10.1007/s005310000149
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Plastic flow of omphacite in eclogites at temperatures below 500°C – implications for interplate coupling in subduction zones.
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- International Journal of Earth Sciences, 2001, v. 90, n. 1, p. 197, doi. 10.1007/s005310000159
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Grain-size-sensitive flow and shear-stress enhancement at the brittle–ductile transition of the continental crust.
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- International Journal of Earth Sciences, 2001, v. 90, n. 1, p. 181, doi. 10.1007/s005310000160
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Strain localization as a key to reconciling experimentally derived flow-law data with dynamic models of continental collision.
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- International Journal of Earth Sciences, 2001, v. 90, n. 1, p. 168, doi. 10.1007/s005310000151
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Relating experimental and geological rheology.
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- International Journal of Earth Sciences, 2001, v. 90, n. 1, p. 157, doi. 10.1007/s005310000158
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Rheology and geodynamic modelling: the next step forward.
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- International Journal of Earth Sciences, 2001, v. 90, n. 1, p. 149, doi. 10.1007/s005310000161
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Textural and microstructural evidence for semi-brittle flow in natural fault rocks with varied mica contents.
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- International Journal of Earth Sciences, 2001, v. 90, n. 1, p. 14, doi. 10.1007/s005310000166
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Weakening and strain localization produced by syn-deformational reaction of plagioclase.
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- International Journal of Earth Sciences, 2001, v. 90, n. 1, p. 136, doi. 10.1007/s005310000148
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Lattice preferred orientation in deformed-then-annealed material: observations from experimental and natural polycrystalline aggregates.
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- International Journal of Earth Sciences, 2001, v. 90, n. 1, p. 127, doi. 10.1007/s005310000163
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Texture development of polycrystalline anhydrite experimentally deformed in torsion.
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- International Journal of Earth Sciences, 2001, v. 90, n. 1, p. 118, doi. 10.1007/s005310000162
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Crystallographic control on the development of foam textures in quartz, plagioclase and analogue material.
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- International Journal of Earth Sciences, 2001, v. 90, n. 1, p. 104, doi. 10.1007/s005310000170
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Deformation of partially molten granite: a review and comparison of experimental and natural case studies.
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- International Journal of Earth Sciences, 2001, v. 90, n. 1, p. 60, doi. 10.1007/s005310000164
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- Article