Kyanite Polymorphism
Kyanite polymorphism is a mineralogical phenomenon within metamorphic petrology wherein the aluminum silicate Al₂SiO₅ exists in a triclinic crystal structure stable under high-pressure, moderate-temperature conditions, distinguishing it from its polymorphic counterparts andalusite and sillimanite.
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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
Chunjing Wei, G. L. Clarke, Wei Tian et al. · Lithos · 2007 · 137 citations
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Universitat Autònoma de Barcelona
Cerdanyola del Vallès, Spain
2 h-index
8 publications
170 citations
Ruhr University Bochum
Bochum, Germany
2 h-index
4 publications
110 citations
University of Cambridge
Cambridge, United Kingdom
2 h-index
3 publications
423 citations
United States Geological Survey
Reston, United States
2 h-index
2 publications
74 citations

University of Minnesota
Minneapolis, United States
2 h-index
4 publications
148 citations
Wuhan University of Technology
Wuhan, China
2 h-index
6 publications
122 citations
Natural History Museum
London, United Kingdom
1 h-index
1 publications
15 citations
United States Army
Arlington, United States
1 h-index
4 publications
44 citations
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7 publications · 248 citations
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4 publications · 155 citations
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3 publications · 212 citations
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3 publications · 224 citations
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2 publications · 89 citations
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