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- W2327071386 abstract "Extensive negative aeromagnetic anomalies in the Modum area, south Norway, derive from rocks containing ilmenite with hematite exsolution, or hematite with ilmenite exsolution, carrying strong/stable reversed remanence. Here we describe a 2.5 cm thick high-temperature metamorphic vein of exsolved titanohematite. Reflected-light and EMP analyses show it contains three types of exsolution: spinel plates on (001); rutile blade satellites on spinel oriented at angles of ~60-90° to titanohematite (001); and lamellae 0.1-0.3 mm thick too fine for EMP analyses, also parallel to (001). Powder XRD gave a = 5.0393 Å, c = 13.7687 Å, V = 302.81 Å3 for titanohematite (≈Ilm9), and unrefined reflections of rutile and geikielite. Overlap EMP analyses showed enrichment in MgO, TiO2, and lack of Al2O3, indicating a mixture of titanohematite and geikielite. Non-overlap analyses showed the titanohematite is 6%Fe2+TiO3, 2%MgTiO3, 92% Fe2O3, generally confirmed by TEM-EDX analyses that also showed the geikielite is 30%Fe2+TiO3, 70%MgTiO3." @default.
- W2327071386 created "2016-06-24" @default.
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- W2327071386 date "2014-08-01" @default.
- W2327071386 modified "2023-09-24" @default.
- W2327071386 title "Ferroan geikielite and coupled spinel-rutile exsolution from titanohematite: Interface characterization and magnetic properties" @default.
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- W2327071386 doi "https://doi.org/10.2138/am.2014.4711" @default.
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