Recycling and transport of continental material through the mantle wedge above subduction zones: A Caribbean example
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文摘

We report on the presence of inherited zircons in Cuban ophiolitic and volcanic rocks.

The zircons most likely derived from northern South America and Mexican terranes.

The detrital grains were likely transported into the mantle via subduction of oceanic crust.

Zircon survival suggests that crustal recycling rates in some arcs may be higher than hitherto realized.

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