Recycling in the subduction factory: Archaean to Permian zircons in the oceanic Cretaceous Caribbean island-arc (Hispaniola) Abstract Little mineralogical evidence is left of the recycling of continental and oceanic crust into the mantle at subduction zones. Zircon, because of its exceptional robustness, is probably the only surviving phase and the best mineral tracer of this…
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Monthly Archives: November 2017
2020: Diamond forms during low pressure serpentinisation of oceanic lithosphere
Diamond forms during low pressure serpentinisation of oceanic lithosphere Abstract Diamond is...
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