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Article
Post-Archean Nb-REE-U enrichment in the Superior craton recorded in metasomatised mantle rocks erupted in the 1.1 Ga Midcontinental Rift event
Mantle xenoliths in a Mesoproterozoic lamprophyre dyke at Elliot Lake, Ontario, located on the east margin of the Midcontinent Rift (MCR), erupted at ~ 1.1 Ga. These xenoliths enable a study of critical metal ...
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Article
Open AccessSublithospheric diamond ages and the supercontinent cycle
Subduction related to the ancient supercontinent cycle is poorly constrained by mantle samples. Sublithospheric diamond crystallization records the release of melts from subducting oceanic lithosphere at 300–7...
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Article
Magmatic origin for the massive sulfide ores in the sedimentary country rocks of mafic–ultramafic intrusions in the Midcontinent Rift System
Some mafic–ultramafic intrusions in the North American Midcontinent Rift System host disseminated to massive sulfides of magmatic origin. Massive sulfides are also present in the immediate sedimentary country ...
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Article
Reply to: Evidence for two blue (type IIb) diamond populations
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Article
Blue boron-bearing diamonds from Earth’s lower mantle
Geological pathways for the recycling of Earth’s surface materials into the mantle are both driven and obscured by plate tectonics1–3. Gauging the extent of this recycling is difficult because subducted crustal c...
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Article
Formation of cratonic subcontinental lithospheric mantle and complementary komatiite from hybrid plume sources
Peridotitic sulphide inclusions in diamonds from the central Slave craton constrain the age and origin of their subcontinental lithospheric mantle (SCLM) sources. These sulphides align with either a ca. 3.5 Ga...
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Article
Diamond formation episodes at the southern margin of the Kaapvaal Craton: Re–Os systematics of sulfide inclusions from the Jagersfontein Mine
Sulfide inclusions in diamonds from the 90-Ma Jagersfontein kimberlite, intruded into the southern margin of the Kaapvaal Craton, were analyzed for their Re–Os isotope systematics to constrain the ages and pet...
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Article
Isotopic and trace element constraints on the petrogenesis of lavas from the Mount Adams volcanic field, Washington
Strontium, Nd, Pb, Hf, Os, and O isotope compositions for 30 Quaternary lava flows from the Mount Adams stratovolcano and its basaltic periphery in the Cascade arc, southern Washington, USA indicate a major co...
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Article
Continental mantle signature of Bushveld magmas and coeval diamonds
Over two billion years ago, the Bushveld Complex, the world's largest layered intrusion and platinum group element repository, was emplaced within the Kaapvaal craton of southern Africa, one of Earth's earlies...
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Article
Three-component isotopic heterogeneity near the Oceanographer transform, Mid-Atlantic Ridge
Tholeiitic basalts collected over an area of less than 100 km2 near the Oceanographer transform fault have isotopic compositions interpreted as mixing between three chemically distinct mantle sources. Of the two ...
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Article
Mantle-derived Archaean monozodiorites and trachyandesites
The 2,680–2,750-Myr old1–5 intrusive granite–greenstone terranes6–8 in the Rainy Lake region, Ontario, and in, and adjacent to, the Vermilion District, Minnesota, of the Superior Province in North America, includ...