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The crystallographic texture of the three main constituting phases of a granodioritic rock have been determined quantitatively, using neutron diffraction with a position sensitive detector. Intensities deconvoluted from the full profiles were used in the orientation distribution refinements using the WlMV algorithm. Satisfactory results were obtained for the three phases.

textures and microstructures

Orientation Distributions of Low Symmetry Polyphase Materials Using Neutron Diffraction Data: Application to a Rock Composed of Quartz, Biotite and Feldspar