Priscoan (4.00-4.03 Ga) orthogneisses from northwestern Canada

Samuel A. Bowring*, Ian S. Williams

*Corresponding author for this work

    Research output: Contribution to journalArticlepeer-review

    468 Citations (Scopus)


    Ancient crustal rocks provide the only direct evidence for the processes and products of early Earth differentiation. SHRIMP zircon U-Th-Pb dating has identified, amongst the Acasta gneisses of the western Slave Province, Canada, two metatonalites and a metagranodiorite that have igneous ages of 4002 ± 4, 4012 ± 6 and 4031 ± 3 Ga respectively. These are the first identified Priscoan terrestrial rocks. A record of metamorphic events at ∼3.75, ∼3.6 and ∼1.7 Ga also is preserved. These discoveries approximately double, to ∼40 km2, the area over which ∼4.0 Ga gneisses are known to occur. A single older zircon core in one sample suggests that rocks as old as 4.06 Ga might yet be found in the region. As early as 4.03 Ga, terrestrial differentiation was already producing tonalitic magmas, probably by partial melting of pre-existing, less differentiated crust.

    Original languageEnglish
    Pages (from-to)3-16
    Number of pages14
    JournalContributions to Mineralogy and Petrology
    Issue number1
    Publication statusPublished - 1999


    Dive into the research topics of 'Priscoan (4.00-4.03 Ga) orthogneisses from northwestern Canada'. Together they form a unique fingerprint.

    Cite this