Crustal evolution in NW Scotland through U-Pb, δ18O and εHf in detrital zircon

Penelope J. Lancaster, Craig D. Storey, Chris J. Hawkesworth

    Research output: Contribution to conferencePaperpeer-review

    45 Downloads (Pure)

    Abstract

    Recent work on the evolution of the Earth’s continental crust has focussed on the ability of refractory minerals, such as zircon, to preserve information about crustal units long since lost from the rock record.
    Original languageEnglish
    Publication statusPublished - 2009
    EventGeological Society of London Fermor Meeting on Rodinia (2009) - London, United Kingdom
    Duration: 7 Sept 20099 Sept 2009

    Conference

    ConferenceGeological Society of London Fermor Meeting on Rodinia (2009)
    Country/TerritoryUnited Kingdom
    CityLondon
    Period7/09/099/09/09

    Fingerprint

    Dive into the research topics of 'Crustal evolution in NW Scotland through U-Pb, δ18O and εHf in detrital zircon'. Together they form a unique fingerprint.

    Cite this