Giant Kiruna-type deposits form by efficient flotation of magmatic magnetite suspensions by Knipping, Jaayke L, Bilenker, Laura D, Simon, Adam C, Reich, Martin, Barra, Fernando, Deditius, Artur P, Lundstrom, Craig, Bindeman, Ilya, Munizaga, Rodrigo

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Kinetics of sulfide mineral oxidation in seawater: Implications for acid generation during in situ mining of seafloor hydrothermal vent deposits by Bilenker, Laura D., Romano, Gina Y., McKibben, Michael A.

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A Systematic Investigation of the Effects of Standard‐Sample Concentration Mismatch during Fe Isotope Measurement by MC‐ICP‐MS by King‐Doonan, Elizabeth K., Bilenker, Laura D., Weis, Dominique, Gordon, Kathy, Fourny, Anaïs, Patton, Genna M., Zhao, Ye

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Iron isotopic evolution during fractional crystallization of the uppermost Bushveld Complex layered mafic intrusion by Bilenker, Laura D., VanTongeren, Jill A., Lundstrom, Craig C., Simon, Adam C.

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Trace elements in magnetite from massive iron oxide-apatite deposits indicate a combined formation by igneous and magmatic-hydrothermal processes by Knipping, Jaayke L., Bilenker, Laura D., Simon, Adam C., Reich, Martin, Barra, Fernando, Deditius, Artur P., Wӓlle, Markus, Heinrich, Christoph A., Holtz, François, Munizaga, Rodrigo

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Fe–O stable isotope pairs elucidate a high-temperature origin of Chilean iron oxide-apatite deposits by Bilenker, Laura D., Simon, Adam C., Reich, Martin, Lundstrom, Craig C., Gajos, Norbert, Bindeman, Ilya, Barra, Fernando, Munizaga, Rodrigo

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Iron isotopic evolution during fractional crystallization of the uppermost B ushveld C omplex layered mafic intrusion by Bilenker, Laura D., VanTongeren, Jill A., Lundstrom, Craig C., Simon, Adam C.

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