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Published in 2019 at "American Mineralogist"
DOI: 10.2138/am-2019-6604
Abstract: Abstract Clinohumite is a potentially abundant silicate mineral with high water concentration (2~3 wt% H2O) that is generated from dehydration of serpentine-group minerals in subduction zones. Previous studies show that fluorine substitution (OH- = F-)…
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Keywords:
situ high;
clinohumite;
subduction zones;
temperature ... See more keywords