Fuchsite and chrome-epidote from Fiskenæsset
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چکیده
منابع مشابه
Melting carbonated epidote eclogites: carbonatites from subducting slabs
Current knowledge on the solidus temperature for carbonated eclogites suggests that carbonatitic liquids should not form from a subducted oceanic lithosphere at sub-arc depth. However, the oceanic crust includes a range of gabbroic rocks, altered on rifts and transforms, with large amounts of anorthite-rich plagioclase forming epidote on metamorphism. Epidote disappearance with pressure depends...
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ژورنال
عنوان ژورنال: Rapport Grønlands Geologiske Undersøgelse
سال: 1976
ISSN: 2597-2944,0418-6559
DOI: 10.34194/rapggu.v73.7423