Isochemical Metamorphism
Isochemical Metamorphism is a type of metamorphic process in which the bulk chemical composition of a rock remains essentially unchanged during mineralogical and textural transformation under conditions of elevated temperature and pressure, distinguished from allochemical metamorphism by the absence of significant chemical mass transfer.
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Carbonic metamorphism, granulites and crustal growth
Robert C. Newton, J. V. Smith, Brian F. Windley · Nature · 1980 · 519 citations
Hideki Wada, Toshihiro Tomita, Kazuhiro Matsuura et al. · Contributions to Mineralogy and Petrology · 1994 · 133 citations
Intersecting Isograds in the Whetstone Lake Area, Ontario
D. M. Carmichael · Journal of Petrology · 1970 · 113 citations
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University of Lausanne
Lausanne, Switzerland
3 h-index
5 publications
135 citations
Nagoya University
Nagoya, Japan
2 h-index
4 publications
220 citations

University of Leicester
Leicester, United Kingdom
2 h-index
3 publications
647 citations
Institute of Geology and Geophysics
Beijing, China
2 h-index
4 publications
350 citations

Chinese Academy of Sciences
Beijing, China
2 h-index
4 publications
350 citations
Universidad Nacional Autónoma de México
Mexico City, Mexico
2 h-index
2 publications
50 citations
Tongji University
Shanghai, China
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3 publications
210 citations
Presidency University
Kolkata, India
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1 publications
26 citations
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4 publications · 122 citations
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4 publications · 141 citations
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JGS · 3 publications · 190 citations
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3 publications · 200 citations
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3 publications · 180 citations
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