Orientation of exsolved pentlandite in natural and synthetic nickeliferous pyrrhotite
Carl A. Francis, Michael E. Fleet, Kamakhya Prakash Misra, James R. Craig
Abstract
Carl A. Francis, Michael E. Fleet, Kamakhya Prakash Misra, James R. Craig
Abstract
Pentlandite (pn), (Fe, Ni)rSB, exsolves from nickeliferous pyrrhotite (po), (Fe, Ni)r-,S, in the form of flames exhibiting weak reflection anisotropism and preferred orientation. X-ray precession studies on both natural and synthetic crystals have established the orientation relation: (111)pnll (00.1)po; (0Tl )pn ll (l 1.0)po; (TT2)pn ll (10.0)po. In synthesis experiments, rapidly quenched samples of (Fe,Ni)r-,S solid solutions contain randomly oriented blebs of pentlandite, whereas slowly cooled charges contain coherent lamellae of pentlandite parallel to (00.1) of pyrrhotite.
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Pentlandite (pn), (Fe, Ni)rSB, exsolves from nickeliferous pyrrhotite (po), (Fe, Ni)r-,S, in the form of flames exhibiting weak reflection anisotropism and preferred orientation. X-ray precession studies on both natural and synthetic crystals have established the orientation relation: (111)pnll (00.1)po; (0Tl )pn ll (l 1.0)po; (TT2)pn ll (10.0)po. In synthesis experiments, rapidly quenched samples of (Fe,Ni)r-,S solid solutions contain randomly oriented blebs of pentlandite, whereas slowly cooled charges contain coherent lamellae of pentlandite parallel to (00.1) of pyrrhotite.
Key concepts: Pentlandite, Pyrrhotite, Geology, Materials science, Mineralogy, Orientation (vector space), Crystallography, Chemistry