Experimental breakdown of staurolite plus inclusions of albite and muscovite at 800 degrees C and 0.1 GPa
- Authors
- Grapes, R.
- Issue Date
- 2월-2011
- Publisher
- MINERALOGICAL SOC
- Keywords
- staurolite; albite; muscovite; low-P/high-T experimental breakdown; hercynite; corundum; mullite; quartz; glass; metastability
- Citation
- MINERALOGICAL MAGAZINE, v.75, no.1, pp.117 - 133
- Indexed
- SCIE
SCOPUS
- Journal Title
- MINERALOGICAL MAGAZINE
- Volume
- 75
- Number
- 1
- Start Page
- 117
- End Page
- 133
- URI
- https://scholar.korea.ac.kr/handle/2021.sw.korea/113209
- DOI
- 10.1180/minmag.2011.075.1.117
- ISSN
- 0026-461X
- Abstract
- Experimental breakdown of staurolite + inclusions of albite and muscovite (representing an aluminous Fe-rich metapelitic composition) occurs within the KNFMASH system at 800 degrees C and 0.1 GPa under fluid-present conditions over periods of 2 days to 8 weeks. The overall melt-producing reaction is staurolite + muscovite + plagioclase + vapour = hercynite + corundum + mullite + quartz + liquid, and involves three reactions; staurolite + vapour = hercynite + corundum + quartz + liquid, albite + vapour = mullite + liquid, and muscovite + vapour = mullite + liquid. Melt (glass) compositions are siliceous (77.2-64.5 wt.% SiO2), peraluminous (A/CNK = 1.5-5.5), and have granite-trondjhemite compositions in terms of normative Ab-Ab-Or contents. Textures indicate that quartz formed later than corundum. The corundum + quartz + hercynite assemblage after staurolite is considered to be metastable and only likely to be found in nature where staurolite-bearing rocks have undergone rapid heating and melting followed by quenching.
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