Abstract
The partition coefficients of V and Sc between clinopyroxene and silicate melt
Acknowlegments
Support from the Recruitment Program of Global Young Experts (PR China) is appreciated. Constructive reviews by Maryjo Brounce, Ian Swainson, and two anonymous reviewers significantly improved this paper.
References cited
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Articles in the same Issue
- Review
- Biosilica as a source for inspiration in biological materials science
- Ab initio study of water speciation in forsterite: Importance of the entropic effect
- Surface-modified phillipsite-rich tuff from the Campania region (southern Italy) as a promising drug carrier: An ibuprofen sodium salt trial
- Structure of low-order hemimorphite produced in a Zn-rich environment by cyanobacterium Leptolingbya frigida
- Formation of dolomite catalyzed by sulfate-driven anaerobic oxidation of methane: Mineralogical and geochemical evidence from the northern South China Sea
- Anisotropic growth of olivine during crystallization in basalts from Hawaii: Implications for olivine fabric development
- Melting experiments on Fe–Si–S alloys to core pressures: Silicon in the core?
- High-pressure phase behavior and equations of state of ThO2 polymorphs
- Mafic inputs into the rhyolitic magmatic system of the 2.08 Ma Huckleberry Ridge eruption, Yellowstone
- Toward the wider application of 29Si NMR spectroscopy to paramagnetic transition metal silicate minerals and glasses: Fe(II), Co(II), and Ni(II) silicates
- Equations of state and phase boundary for stishovite and CaCl2-type SiO2
- Insight on gem opal formation in volcanic ash deposits from a supereruption: A case study through oxygen and hydrogen isotopic composition of opals from Lake Tecopa, California, U.S.A
- Revisiting the crystal structure of dickite: X-ray diffraction, solid-state NMR, and DFT calculations study
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- Letter
- Why natural monazite never becomes amorphous: Experimental evidence for alpha self-healing
- New Mineral Names
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