Titlebook: ;

極小

終點

Homogeneity of Granite Fabrics at the Metre and Dekametre Scales such as a C/S system was observed. The magnetic anisotropy and the bulk susceptibility are homogeneous as a whole, and display spatial organizations with no simple relationships with the structures. These results confirm, however, the validity of the homogeneous structural patterns obtained from en

comely

Analogue 3D Simple-Shear Experiments of Magmatic Biotite Subfabricst rotate as much and deviates 10° from that expected. For larger shear strains, the fabrics are consistently oriented, but a 10° offshear-plane deviation remains. From these experiments we conclude that, even at low concentrations of crystals, magmatic biotite subfabrics are not expected to behave c

GROG

Interferons

Rigid Particles in Simple Shear Flow: Is Their Preferred Orientation Periodic or Steady-State ?/matrix interface may not always be coherent; and (iii) the aspect ratios of the crystals defining the SPO are unlikely to be unique and constant, as assumed in the model. The last point is discussed on the basis of some 2D simple calculations of the development of SPO defined by different types of

后來

無法取消

Granite Pluton Geometry and Emplacement Mode Inferred from Combined Fabric and Gravity Datafeeder zones. They are emplaced as sills in the upper crust, or within rather ductile environments in extensionnal tectonic contexts. These contrast with the thick (more than 10 kilometres) wedge-shaped plutons, extending largely in one direction along which a few root zones appear, which are V-shap

Solace

帶傷害

Development of Magmatic to Solid-State Fabrics during Syntectonic Emplacement of the Mono Creek Granprovide semi-quantitative information: K correlates with rock mineralogy, and P is a good indicator of the rock texture. The AMS directional data of the MCG are characterized by good clustering at each sampling station, and by a sigmoidal pattern of foliation and lineation. This pattern results from

Vo2-Max