Spinel peridotite xenoliths from the Tariat Depression, Mongolia. I: Major element chemistry and mineralogy of a primitive mantle xenolith suite
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2022, Geochimica et Cosmochimica ActaMetasomatism of the off-cratonic lithospheric mantle beneath Hangay Dome, Mongolia: Constraints from trace-element modelling of lherzolite xenoliths
2021, LithosCitation Excerpt :Sample ST0802 displays a unique medium-grained tabular microstructure characterized by up to 5 mm long tabular olivine crystals, irregular shaped orthopyroxene, and smaller clinopyroxene with common spinel inclusions. In general, these observations are consistent with previous studies, which also found medium to coarse grained protogranular to granoblastic slightly depleted spinel lherzolites in the same localities (Ionov (1986, 2007), Preβ et al. (1986), Ionov et al. (1998), Ionov and Hofmann (2007), Carlson and Ionov (2019), and Demouchy et al. (2019)). These works noted the presence of very rare (1%) phlogopite, amphibole, apatite, alkali feldspar, and interstitial silicate glass.
Potassium distribution and isotope composition in the lithospheric mantle in relation to global Earth's reservoirs
2021, Geochimica et Cosmochimica ActaCitation Excerpt :Fresh kimberlite K-27-04 from the Udachnaya pipe on the Siberian craton (Kamenetsky et al., 2012) has δ41K = −0.40 ± 0.07‰. Three samples (vesicular lava, glass fragment and phlogopite megacryst) from the Shavaryn-Tsaram volcanic breccia in Tariat (Press et al., 1986) show a δ41K range of −0.47‰ to −0.27‰ (av. −0.40 ± 0.18‰).