Grain‐size dependence of the rock magnetic properties for a natural maghemite
- 1 October 1996
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 23 (20), 2815-2818
- https://doi.org/10.1029/96gl00781
Abstract
No abstract availableThis publication has 18 references indexed in Scilit:
- Temperature dependence of the hyperfine parameters of maghemite and al-substituted maghemitesPhysics and Chemistry of Minerals, 1995
- The infrared dielectric properties of maghemite, ?-Fe2O3, from reflectance measurement on pressed powdersPhysics and Chemistry of Minerals, 1995
- High-temperature hysteresis and thermoremanence of single-domain maghemitePhysics of the Earth and Planetary Interiors, 1990
- Identification of ferromagnetic minerals in a rock by coercivity and unblocking temperature propertiesGeophysical Research Letters, 1990
- Magnetic properties of natural pyrrhotite Part I: Behaviour of initial susceptibility and saturation-magnetization-related rock-magnetic parameters in a grain-size dependent frameworkPhysics of the Earth and Planetary Interiors, 1988
- Transformation of Trace Element-Substituted Maghemite to HematiteClays and Clay Minerals, 1988
- The Influence of Aluminum on Iron Oxides: XI. Aluminum‐Substituted Maghemite in Soils and Its FormationSoil Science Society of America Journal, 1984
- Interacting vs. non-interacting single domain behavior in natural and synthetic samplesPhysics of the Earth and Planetary Interiors, 1981
- MAGNETIC SUSCEPTIBILITY OF THE SOIL AND ITS SIGNIFICANCE IN SOIL SCIENCE – A REVIEWEuropean Journal of Soil Science, 1977
- Hysteresis properties of titanomagnetites: Grain-size and compositional dependencePhysics of the Earth and Planetary Interiors, 1977