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- W2892615535 abstract "Abstract The veins in the mantle wedge peridotite can record the activity of slab-derived melt/fluid, which is the reflection of the material circulation between crust and mantle. A red-corundum-bearing vein is present in the Rai–Iz ultramafic rocks in the Polar Urals, Russia. The ultramafic rocks are harzburgite and dunite, and the red corundum-bearing rocks consist of phlogopite, paragonite, oligoclase, red corundum, and chromian spinel. Red corundum occurs as prophyroblasts or fine grains that contain 92–98 wt% Al2O3 and 2–7 wt% Cr2O3. Chromian spinel has Cr# values ([100Cr/ (Cr + Al)] atomic ratio) of 46–78. Oligoclase is characterized by An values of 20–30. Phlogopite is Ba-rich (BaO = 0.8–2.7 wt%) and paragonite is Sr-rich (SrO = 0.8–2.3 wt%). Zircons from the oligoclasite show oscillatory zoning and Th/U values of" @default.
- W2892615535 created "2018-10-05" @default.
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- W2892615535 date "2018-11-01" @default.
- W2892615535 modified "2023-09-27" @default.
- W2892615535 title "A red-corundum-bearing vein in the Rai–Iz ultramafic rocks, Polar Urals, Russia: the product of fluid activity in a subduction zone" @default.
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- W2892615535 doi "https://doi.org/10.1016/j.lithos.2018.09.025" @default.
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