Magnetic fabrics show an evolution similar to the silicate mineral fabrics.
Magnetic fabrics show an evolution similar to the silicate mineral fabrics in general.
The presence of -type fabrics around some of these phenocrysts implies top-to-the-west flow.
Many kinematic indicators (primarily - and type fabrics) show that the shear zone has an extensional geometry with respect to the present land surface.
Relative rheology of coeval mafic and felsic magmas: nature of resulting interaction processes and shape and mineral fabrics of mafic microgranular enclaves.
The studies presented above show that fabrics both at the northern contact of the batholith and inside the batholith formed during oblate coaxial deformation.
Discussion: crossed girdle c-axis fabrics in quartzites plastically deformed by plain strain and in progressive simple shear.
Knitted fabrics; knit type, wale, and course count per linear inch.
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