Sillimanite Polymorphism
Sillimanite Polymorphism is a mineralogical phenomenon within metamorphic petrology wherein the aluminosilicate mineral sillimanite exhibits distinct crystalline structures under varying temperature and pressure conditions, representing a specific type of phase transition among polymorphs in the Al₂SiO₅ system.
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The pressure–temperature–time path of migmatites from the Sikkim Himalaya
Nigel Harris, Mark J. Caddick, Jan Košler et al. · Journal of Metamorphic Geology · 2004 · 180 citations
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University of Cambridge
Cambridge, United Kingdom
3 h-index
5 publications
435 citations
University College London
London, United Kingdom
2 h-index
2 publications
48 citations

Pennsylvania State University
State College, United States
2 h-index
6 publications
350 citations
Charles University
Prague, Czechia
1 h-index
1 publications
180 citations

Royal Geographical Society
London, United Kingdom
1 h-index
1 publications
11 citations
Virginia Tech
Blacksburg, United States
1 h-index
1 publications
10 citations
Institute of Mineralogy
Miass, Russia
1 h-index
1 publications
32 citations

TU Wien
Vienna, Austria
1 h-index
2 publications
34 citations
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2 publications · 118 citations
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2 publications · 201 citations
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