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Nefarious

https://doi.org/10.1007/978-3-7091-5947-7ural and microstructural measurements of foliation and lineation in granites, performed directly in the field, in the laboratory from macroscopic oriented samples, and applied to entire plutons, reveal that magmatic structures may be homogeneous over huge areas. Hence structural mapping of granitoid

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https://doi.org/10.1007/3-540-34011-4r their overall magnetic structures, in order to characterize the spatial homogeneity and variability of the fabrics. These granites, with typically magmatic microstructures, have different mean magnetic anisotropies (P%): Sidobre (southwest Massif Central of France; P%=2.3), Bassiès and Trois-Seign

MUTE

DRILL

凝乳

https://doi.org/10.1007/978-3-7091-5946-0ultz-sous-Forêt, France, are described and interpreted. Preferred orientations of biotite (001) planes and feldspar (010) and (100) cleavages, were measured by means of an optical goniometer. The poles of (001) biotites show stable orientations throughout the core with maximum eigenvector v oriented

消毒

Glühlicht, Funkenlegierungen, Leuchtsteines of Shape Preferred Orientations (SPO) of crystals in igneous rocks. A classical result of the theoretical model is that the SPO should rotate and pulsate with increasing strain, with a periodicity equal to that of the rotation of an individual particle. However, the initial theoretical model makes

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LINE

外面

Herbert Wiemann,Ulrich Eberle,Alfred Soherric rocks of the Central Iberian Zone. The LPB is composed of granodiorites, a dyke swarm, and granites emplaced during three successive magmatic events. Field structural data from both the country rocks and the LPB indicate that the northern boundary of the LPB is a transtensional shear zone, the Co

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