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- W289553887 abstract "The Chugach Metamorphic Complex (CMC, Alaska) is a 200 km long and 10-50 km wide complex and is part of an active accretionary prism. According to the sparse existing literature, the complex is believed to be a lowpressure high-temperature terrain (400-650°C and ∼3kb) with a migmatitic inner core (∼5-10 km) and schist rims surrounded by phyllite (Sisson et al., 1988). Such low pressure conditions are not common in a subduction zone setting and the formation of the complex is thus attributed to the subduction of a ridge during the Eocene (∼ 50 my)." @default.
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- W289553887 date "2010-05-01" @default.
- W289553887 modified "2023-09-23" @default.
- W289553887 title "Metamorphism of the Chugach Metamorphic Complex, (Alaska). New pressure estimates question the ridge subduction context." @default.
- W289553887 hasPublicationYear "2010" @default.
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