FeTi oxide mineralogy and the origin of normal and reverse remanent magnetization in dacitic pumice blocks from Mt. Shasta, California
- 30 June 1987
- journal article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 46 (1-3), 270-288
- https://doi.org/10.1016/0031-9201(87)90190-7
Abstract
No abstract availableKeywords
This publication has 19 references indexed in Scilit:
- An SEM study of phyllosilicates in a Westphalian Coal Measures sandstone using back-scattered electron imaging and wavelength dispersive spectral analysisSedimentary Geology, 1984
- Remanent magnetization of a “paramagnetic” composition in the ilmenite‐hematite solid solution seriesGeophysical Research Letters, 1984
- Alternating field characteristics of pseudo-single-domain (2–14 μm) and multidomain magnetiteEarth and Planetary Science Letters, 1983
- Antiphase Domains and Reverse Thermoremanent Magnetism in Ilmenite-Hematite MineralsScience, 1981
- Magnetic properties and oxidation of iron-titanium oxide minerals in Alae and Makaopuhi Lava Lakes, HawaiiJournal of Geophysical Research, 1969
- Empirical Correction Factors for the Electron Microanalysis of Silicates and OxidesThe Journal of Geology, 1968
- The iron-titanium oxides of salic volcanic rocks and their associated ferromagnesian silicatesContributions to Mineralogy and Petrology, 1966
- Iron-Titanium Oxide Minerals and Synthetic EquivalentsJournal of Petrology, 1964
- Magnetic Properties of Ilmenite-Hematite System at Low TemperatureJournal of the Physics Society Japan, 1962
- An Order-Disorder Transformation Phenomenon in the FeTiO3–Fe2O3 Solid Solution SeriesJournal of the Physics Society Japan, 1958