Precambrian Zircons in Chromitites of the Cretaceous Aladag Ophiolite (Turkey) Indicate Deep Crustal Recycling in Oceanic Mantle

Precambrian Research, pp. 1058382020.

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Abstract Crustal recycling into Earth’s deep mantle has been inferred from both seismic tomography and geochemical observations. As a further line of evidence, we report on zircons having a wide range of ages that were recovered from the Aladag chromitites, providing direct evidence for crustal recycling. Mesozoic zircons represent the ...More



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