Age, origin, and thermal evolution of the ultra-fresh ~1.9Ga Winnipegosis Komatiites, Manitoba, Canada
Research output: Contribution to journal › Journal article › Research › peer-review
Pedro Waterton, D. Graham Pearson, Bruce Kjarsgaard, Larry Hulbert, Andrew Locock, Stephen Parman, Bill Davis
The Proterozoic spans the longest portion of earth's history, yet in contrast to the Archaean, the record of komatiites and related high MgO igneous rocks from this Eon is sparse. This paper describes the pristine Palaeoproterozoic Winnipegosis Komatiites, from Manitoba, Canada, which form part of the Circum-Superior Belt large igneous province. We present a comprehensive petrographical investigation, mineral and bulk rock geochemistry, and Al-in-olivine thermometry for the Winnipegosis Komatiites, along with new U-Pb SHRIMP dating of zircons from a mafic unit, which yield an age of 1870.3±7.1Ma for the Winnipegosis Komatiite Belt. The komatiites are Al-undepleted and dominated by massive olivine porphyritic flows with a median thickness of 6m. Differentiated flows containing layers of olivine spinifex are present, but rare. Trace element data indicate the komatiites were derived from depleted mantle, and subsequently contaminated with 2–3% continental crust. Temperatures from Al-in-olivine thermometry are consistent with a nominally dry melt, and combined with olivine-melt Mg–Fe partitioning, suggest a parental melt with ~24wt% MgO and a liquidus (olivine) temperature of ~1501°C, approximately 100°C cooler than their hottest Archaean counterparts. At ~1424°C chromite joined olivine as a crystallising phase. Olivine and chromite phenocrysts were re-mixed with residual melt shortly before or during komatiite eruption, which occurred by the time the magma had cooled to ~1321°C. Combined geochemical and geological evidence requires that the Winnipegosis Komatiites erupted onto rifting continental crust. Their high liquidus temperatures require anomalously hot mantle. Considering the Winnipegosis Komatiites in the context of the broader Circum-Superior Belt, we suggest that these magmas formed from a mantle plume that was deflected towards the margins of the Superior craton by strong gradients in lithospheric thickness. This interpretation of the mode of formation of the Circum-Superior Belt casts doubt on ambient mantle potential temperatures as high as 1600°C during the Proterozoic.
|Pages (from-to)||114 - 130|
|Number of pages||17|
|Publication status||Published - 2017|
- The Faculty of Science - Proterozoic, Komatiite, Circum-Superior Belt, Trans-Hudson Orogeny, Al-in-olivine thermometer, Mantle potential temperature