DOI: 10.1186/s13568-014-0094-z Iron is one of the most abundant elements in the biosphere, naturally occurring in the form of various Fe(II)- and Fe(III)-bearing minerals and In addition, very little is known about the reduction of Fe(III) minerals by Chemosphere 79:426 433PubMedView ArticleGoogle Scholar
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Fe2+ in Fe-bearing pyrope garnet with two distinct compositions, (Mg0.8Fe0.2)3Al2Si3O12 (py80alm20) Keywords: Fe-bearing pyrope, Mössbauer spectroscopy, high pressure, high temperature, hyper American Mineralogist, 92, 433 436. Lin, J.F., Alp, E.E., Mao, Z., Inoue, T., McCammon, C., Xiao, Y., Chow, P., and.
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A Tertiary Carbon Iron Bond as an FeCl Synthon and the Reductive . Chemoselective Reactions of (E)-1,3-Dienes: Cobalt-Mediated Isomerization to (Z)-1,3-Dienes and Reactions with Ethylene .. ACS Catalysis 2012 2 (3), 433-440.
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