Zoned quartz phenocrysts in supercooled melt inclusions in granulites from continental collision orogens
Felsite inclusions (FIs) in granulite garnets from continental collision orogens are supercooled felsic melt inclusions. Not only do these represent non-equilibrium textures, such as dendritic and spherulitic crystals of quartz and other minerals, but the porphyritic texture is that of hypabyssal and volcanic rocks. This paper presents representative zoned quartz phenocryst-bearing FIs in various granulites from the Highland Complex in central Sri Lanka, the Lützow-Holm Complex in East...[Show more]
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|Source:||The Island Arc|
|Island Arc - 2020 - Hiroi - Zoned quartz phenocrysts in supercooled melt inclusions in granulites from continental.pdf||9.83 MB||Adobe PDF||Request a copy|
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