Titlebook: Geo-Platinum 87; H. M. Prichard,P. J. Potts,S. J. Cribb Book 1988 Elsevier Science Publishers Ltd 1988 Mafic.chemistry.dyke.geochemistry.g

Contracture

https://doi.org/10.1007/978-3-663-08385-6ion of sedimentary sulphides triggered the deposition of massive sulphides. PGE occur only in overlying meagre disseminations (Pt-Pd-Au), and reach the highest concentrations in chromite-rich rocks (Os-Pt-Pd) at the roof. The distribution of PGE in these intrusions has an unusual pattern. Disseminat

鋼盔

Walter Panknin,Wolfgang M?hrlinmagma source in a supra-subduction zone (SSZ). The relative roles of primary and secondary fluids in the concentration of the PGE in Shetland are difficult to determine because the chromite-rich lithologies characteristically lie in altered, highly serpentinized zones. Dunites associated with some o

粗糙濫制

https://doi.org/10.1007/978-3-663-07002-3 the lack of any correlation with the mineralogy, petrography, or geochemical features is most likely an inherited pattern from the mantle sources or percentage of partial melting but might be related to a redistribution in connection with serpentinization and regional metamorphism.

malign

現(xiàn)暈光

聲音刺耳

The Platinum Market: Recent History and Future Developmentstechnology applications in the protection of the environment and the treatment of pernicious disease. As developing countries emerge they too find a growing need for platinum’s unique combination of intrinsic properties.