Abstract
We conducted experiments on an alkali basalt at 1-atmosphere in order to investigate the effects of temperature cycling on crystal coarsening. Experiments at 1,150 °C near the Ni–NiO buffer indicate that coarsening of plagioclase and olivine crystals is greatly accentuated by temperature cycling. For a given experiment duration, crystal number density decreases with temperature cycle amplitude and average crystal size increases with increasing amplitude. We observed little correlation between cycle period and crystal number density or average crystal size. We suggest that dissolution and size-proportional crystal growth during repeated heating and cooling decrease crystal number density and increase average crystal size. These experiments indicate that the texture of silicate minerals can be modified by temperature cycling and that phenocrysts may develop quicker in silicate magmas when the magma temperature is cycled.
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Acknowledgments
This research was supported by National Science Foundation Grant EAR-1052813. The Martin Fund of the Department of Geological Sciences at the University of North Carolina, the Geological Society of America, Sigma Xi, and the Mary Lily Kenan Flagler Bingham Professorship. R.M. acknowledges the NASA Postdoctoral Program and Justin Simon for support. Colin McKinney provided expertise with control systems. Kent Ross assisted with the FE-SEM work. Informal reviews by Alan Boudreau, Drew Coleman, Ryan Frazer, and Breck Johnson on earlier versions of this manuscript helped clarify the content. Journal reviews by Ariel Provost, Pietro Armienti, and editor Jon Blundy greatly improved the quality of the final publication. We also thank Jon Blundy for his editorial handling of the manuscript.
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Mills, R.D., Glazner, A.F. Experimental study on the effects of temperature cycling on coarsening of plagioclase and olivine in an alkali basalt. Contrib Mineral Petrol 166, 97–111 (2013). https://doi.org/10.1007/s00410-013-0867-4
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DOI: https://doi.org/10.1007/s00410-013-0867-4