Continental crust formation by crustal delamination in subduction zones and complementary accumulation of the enriched mantle I component in the mantle
نویسندگان
چکیده
منابع مشابه
Continental crust formation at arcs, the arclogite ‘‘delamination’’ cycle, and one origin for fertile melting anomalies in the mantle
The total magmatic output in modern arcs, where continental crust is now being formed, is believed to derive from melting of the mantle wedge and is largely basaltic. Globally averaged continental crust, however, has an andesitic bulk composition and is hence too silicic to have been derived directly from the mantle. It is well known that one way this imbalance can be reconciled is if the paren...
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Mid-mantle anisotropy in subduction zones and deep water transport
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ژورنال
عنوان ژورنال: Geochemistry, Geophysics, Geosystems
سال: 2000
ISSN: 1525-2027
DOI: 10.1029/2000gc000094