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doi:10.2204/iodp.proc.303306.209.2009 ReferencesDay, R., Fuller, M., and Schmidt, V.A., 1977. Hysteresis properties of titanomagnetites: grain-size and compositional dependence. Phys. Earth Planet. Inter., 13(4):260–267. doi:10.1016/0031-9201(77)90108-X Karlin, R., and Levi, S., 1983. Diagenesis of magnetic minerals in recent hemipelagic sediments. Nature (London, U. K.), 303(5915):327–330. doi:10.1038/303327a0 Özdemir, Ö., Dunlop, D.J., and Moskowitz, B.M., 1993. The effect of oxydation on the Verwey transition in magnetite. Geophys. Res. Lett., 20(16):1671–1674. doi:10.1029/93GL01483 Verwey, E.J.W., 1939. Electronic conduction of magnetite (Fe3O4) and its transition point at low temperatures. Nature (London, U. K.), 144(3642):327–328. doi:10.1038/144327b0 |