Subduction-zone Metamorphism
Subduction-Zone Metamorphism is a type of regional metamorphism characterized by high-pressure, low-temperature conditions that occur in convergent plate boundaries where oceanic crust and sediments are subducted to depth, resulting in the formation of diagnostic mineral assemblages such as lawsonite, glaucophane, and jadeite within metamorphic rocks.
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Metamorphic chemical geodynamics in continental subduction zones
Yong‐Fei Zheng · Chemical Geology · 2012 · 639 citations
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Centre National de la Recherche Scientifique
Paris, France
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110 publications
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Chinese Academy of Sciences
Beijing, China
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123 publications
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Institute of Geology and Geophysics
Beijing, China
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Stanford University
Stanford, United States
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China University of Geosciences
Wuhan, China
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Chinese Academy of Geological Sciences
Beijing, China
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59 publications
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University of Science and Technology of China
Hefei, China
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Australian National University
Canberra, Australia
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