FeTi oxide mineralogy and the origin of normal and reverse remanent magnetization in dacitic pumice blocks from Mt. Shasta, California

Author:

Lawson Charles A.,Nord Gordon L.,Champion Duane E.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics

Reference41 articles.

1. New (and final) models for the Ti-magnetite/ilmenite geothermometer and oxygen barometer;Andersen;Am. Geophys. Union, Trans.,1985

2. Alternating field characteristics of pseudo-single domain (2–14 μm) and multidomain magnetite;Bailey;Earth Planet. Sci. Lett.,1983

3. Empirical correction factors for the electron microanalysis of silicates and oxides;Bence;J. Geol.,1968

4. Iron-titanium oxide minerals and synthetic equivalents;Buddington;J. Petrol.,1964

5. The iron-titanium oxides of sialic volcanic rocks and their associated ferromagnesian silicates;Carmichael;Contrib. Mineral. Petrol.,1967

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