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Halgedahl, S. L., Day, R., Fuller, M. (1980) The effect of cooling rate on the intensity of weak-field trm in single-domain magnetite. Journal of Geophysical Research: Solid Earth, 85. 3690-3698 doi:10.1029/jb085ib07p03690

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Reference TypeJournal (article/letter/editorial)
TitleThe effect of cooling rate on the intensity of weak-field trm in single-domain magnetite
JournalJournal of Geophysical Research: Solid Earth
AuthorsHalgedahl, S. L.Author
Day, R.Author
Fuller, M.Author
Year1980 (July 10)Volume85
PublisherAmerican Geophysical Union (AGU)
DOIdoi:10.1029/jb085ib07p03690Search in ResearchGate
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Mindat Ref. ID903657Long-form Identifiermindat:1:5:903657:8
GUID0
Full ReferenceHalgedahl, S. L., Day, R., Fuller, M. (1980) The effect of cooling rate on the intensity of weak-field trm in single-domain magnetite. Journal of Geophysical Research: Solid Earth, 85. 3690-3698 doi:10.1029/jb085ib07p03690
Plain TextHalgedahl, S. L., Day, R., Fuller, M. (1980) The effect of cooling rate on the intensity of weak-field trm in single-domain magnetite. Journal of Geophysical Research: Solid Earth, 85. 3690-3698 doi:10.1029/jb085ib07p03690
In(1980) Journal of Geophysical Research: Solid Earth Vol. 85. American Geophysical Union (AGU)

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Biggin, A. J., Badejo, S., Hodgson, E., Muxworthy, A. R., Shaw, J., Dekkers, M. J. (2013) The effect of cooling rate on the intensity of thermoremanent magnetization (TRM) acquired by assemblages of pseudo-single domain, multidomain and interacting single-domain grains. Geophysical Journal International, 193 (3) 1239-1249 doi:10.1093/gji/ggt078
Dunlop, David J., Xu, Song, Heider, Franz (2004) Alternating field demagnetization, single-domain-like memory, and the Lowrie-Fuller test of multidomain magnetite grains (0.6-356 μm) Journal of Geophysical Research: Solid Earth, 109. doi:10.1029/2004jb003006
Brown, Elizabeth McClelland (1984) Experiments on TRM intensity dependence on cooling rate. Geophysical Research Letters, 11 (3) 205-208 doi:10.1029/gl011i003p00205
Halgedahl, Susan L. (1998) Revisiting the Lowrie–Fuller test: alternating field demagnetization characteristics of single-domain through multidomain glass–ceramic magnetite. Earth and Planetary Science Letters, 160 (3) 257-271 doi:10.1016/s0012-821x(98)00085-5
Boyd, J. R., Fuller, M., Halgedahl, S. (1984) Domain wall nucleation as a controlling factor in the behaviour of fine magnetic particles in rocks. Geophysical Research Letters, 11 (3) 193-196 doi:10.1029/gl011i003p00193
Bukowinski, M. S. T. (1980) Effect of pressure on bonding in MgO. Journal of Geophysical Research: Solid Earth, 85. 285-292 doi:10.1029/jb085ib01p00285
Moskowitz, Bruce M., Halgedahl, Susan L. (1987) Theoretical temperature and grain-size dependence of domain state in X = 0.6 titanomagnetite. Journal of Geophysical Research: Solid Earth, 92. 10667-10682 doi:10.1029/jb092ib10p10667
Williams, Wyn, Muxworthy, Adrian R., Paterson, Greig A. (2006) Configurational anisotropy in single-domain and pseudosingle-domain grains of magnetite. Journal of Geophysical Research: Solid Earth, 111. doi:10.1029/2006jb004556
Geissman, John Wm. (1980) Paleomagnetism of ash-flow tuffs: Microanalytical recognition of TRM components. Journal of Geophysical Research: Solid Earth, 85. 1487-1499 doi:10.1029/jb085ib03p01487
Siscoe, George L., Sibeck, David G. (1980) Effects of nondipole components on auroral zone configurations during weak dipole field epochs. Journal of Geophysical Research: Solid Earth, 85. 3549-3556 doi:10.1029/jb085ib07p03549
Halgedahl, Susan L. (1995) Bitter patterns versus hysteresis behavior in small single particles of hematite. Journal of Geophysical Research: Solid Earth, 100. 353-364 doi:10.1029/93jb01228
 
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