The effect of metamorphic fluid flow on the nucleation and growth of garnets from Troms, North Norway

• Published in: Journal of Metamorphic Geology
• Main Author: SKELTON, A. D. L.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 1997
• Subjects: Norway; North Norway; Troms
• Online Access: http://dx.doi.org/10.1111/j.1525-1314.1997.t01-1-00051.x; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1525-1314.1997.t01-1-00051.x; https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1525-1314.1997.t01-1-00051.x

A spatial association is observed between the size distribution of garnet porphyroblasts and the size distribution of quartz veins in greenschist facies metapelites from Troms, North Norway. The size distribution of quartz veins reflects the flow regime of metamorphic fluids. The hypothesis that the flow regime of metamorphic fluids is also responsible for the size distribution of garnet crystals was tested by ascribing empirical acceleration parameters to the nucleation and growth rates of garnet crystals. In regions where fluid flow was interpreted as pervasive’, acceleration parameters for nucleation were high, whereas in regions where fluid flow was interpreted as channelled’, acceleration parameters for growth were high. Accelerated crystal growth is further implied from the chemical zoning and crystal morphologies of garnets collected near discrete veins. This spatial association may imply that fluid flow can be instrumental in controlling garnet crystallization. Fluid flow could affect garnet crystallization kinetics by facilitating thermal advection and/or mass transfer. In the study area, rhodochrosite (MnCO 3 ) veins provide evidence for mass transfer of Mn by fluid flow. An influx of Mn would expand the stability field of garnet to lower temperatures. The resulting thermal overstep could accelerate nucleation and/or growth of garnets. The corollary of this study is that size distributions and chemical zoning of garnets, or other porphyroblast phases, can be used to study metamorphic fluid flow.