Diffusion‐controlled olivine corona textures in granitic rocks from Lofoten, Norway: calculation of Onsager diffusion coefficients, thermodynamic modelling and petrological implications

• Published in: Journal of Metamorphic Geology
• Main Authors: MARKL, G., FOSTER, C. T., BUCHER, K.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 1998
• Subjects: Lofoten; Norway
• Online Access: http://dx.doi.org/10.1111/j.1525-1314.1998.00156.x; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1525-1314.1998.00156.x; https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1525-1314.1998.00156.x

Reactions occurring during cooling of charnockitic intrusives on the Lofoten Islands produce characteristic diffusion‐controlled textures around fayalite and Fe–Ti oxides. Thermobarometry indicates the corona textures formed at 780–840 °C and pressures of 4–10 kbar, whereas the magmatic assemblage of the charnockite (clinopyroxene–olivine–quartz) crystallized at about 850–870 °C and 4 kbar. The succession olivine|orthopyroxene+magnetite|orthopyroxene+garnet and olivine|orthopyroxene+magnetite|amphibole developed where olivine reacted with adjacent plagioclase or K‐feldspar, but the modes and the thicknesses of the corona textures vary according to the feldspar type, indicating that the primary magmatic ternary feldspar was already exsolved into albitic plagioclase and alkali feldspar when the corona formation began. Simultaneously, in other parts of the rock, primary magmatic clinopyroxene reacted to amphibole and Fe–Ti oxides reacted to orthopyroxene+garnet coronas or to amphibole. Textures demonstrate significant Al diffusion in the rocks under granulite facies conditions and they suggest that no pervasive fluid influx occurred and that amphibole formation was dependant on a local source of H 2 O probably related to water‐release during the last stages of magmatism. Calculation of the net reaction by accounting for all observed reactions at different sites in the rock indicates that the system can be regarded as balanced on a hand‐specimen scale with respect to all elements except for Na and H 2 O. The larger variety of textures developed in rocks of granitic bulk composition provide more constraints than textures from gabbroic compositions , and permitted calculation of a set of relative diffusion coefficients which also reproduce textures in the gabbroic and anorthositic rocks from the Lofoten Islands. The following set of relative diffusion coefficients (L i /L Fe ) reproduces the observed textures in the Lofoten rocks: Si=0.82, Mg=0.59, Mn=0.05, Na=0.38, K=0.39, Al=0.05 and Ca=0.07.