Boninites as windows into trace element mobility in subduction zones
Boninites are subduction-related rocks originating from re-melting of highly depleted mantle sources left after extraction of tholeiitic melts. Due to their depleted nature, the incompatible trace element inventory of boninites is virtually entirely inherited from slab components without a significa...
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Veröffentlicht in: | Geochimica et cosmochimica acta 2010-01, Vol.74 (2), p.684-704 |
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