Abstract
Many studies have reported U-Pb dates of zircon that are older than the igneous rocks that contain them, and they are therefore thought to be inherited from older rock complexes. Their presence has profound geodynamic implications and has been used to hypothesize about concealed micro-continents, continental crust beneath ocean islands, and recycling of continental material in the mantle beneath mid-ocean ridges. Here, we combine single zircon U-Pb dates and structural radiation damage determined by Raman spectroscopy from a Pliocene mid-ocean ridge gabbro and from Cenozoic igneous rocks to test whether radiation damage allows distinction between contamination and truly inherited zircon. We find that Precambrian zircon found in the Pliocene sample has accumulated substantially more radiation damage than could be explained if they had truly been inherited. In the Cenozoic samples, however, we find that the radiation damage of old grains corresponds with that of young magmatic zircon, suggesting they are genuinely inherited.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
