Abstract
Thermoremanent magnetization (TRM), the dominant mechanism in igneous rocks, has been investigated for many years, yielding a large data base of experimental results and several theoretical models. However, there are still a large number of discrepancies between the observations and the theories.
ArticleNote
Paper presented at the special session on the ‘Origin of TRM,’ American Geophysical Union, San Franscisco, December 9, 1976.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
References
Amar, H., On the width and energy of domain walls in small multi-domain particles, J. Appl. Phys., 28, 732–733, 1957.
Amar, H., Size dependence of the wall characteristics in a two-domain iron particle, J. Appl. Phys., 29, 542–543, 1958a.
Amar, H., Magnetization mechanism and domain structure of multi-domain particles, Phys. Rev., 111, 149–153, 1958b.
Bailey, M. E., The magnetic properties of PSD grains, M.S. thesis, University of Toronto, 1975.
Bailey, M. E., D. J. Dunlop, and K. L. Buchan, Alternating field demagnetization characteristics of pseudo-single-domain grains, EOS, 56, 353, 1975.
Banerjee, S. K., On the origin of stable remanence in pseudo single-domain grains, J. Geomag. Geoelectr., 29, 319–329, 1977.
Bean, C.P. and J. D. Livingston, Superparamagnetism, J. Appl. Phys., 30, 120S–129S, 1959.
Berkowitz, A. E. and W. J. Schuele, Magnetic properties of some ferrite micropowders, J. Appl. Phys., 30, 134S, 1959.
Brown, W. F., Relaxational behavior of fine magnetic particles, J. Appl. Phys., 30, 130S, 1959.
Butler, R. F. and S. K. Banerjee, Theoretical single-domain grain size range in magnetite and titanomagnetite, J. Geophys. Res., 80, 4049–4058, 1975.
Day, R., The effect of grain size on the magnetic properties of the magnetite-ulvospinel solid solution series, Thesis, Univ. of Pittsburgh, Pittsburgh, Pa., 1973.
Day, R., Some curious thermomagnetic curves and their interpretation, Earth Planet. Sci. Lett., 27, 95, 1975.
Day, R., M. D. Fuller, and V. A. Schmidt, Magnetic hysteresis properties of synthetic titanomagnetites, Geophys. Res., 81, 873, 1976.
Day, R., M. D. Fuller, and V. A. Schmidt, Hysteresis properties of titanomagnetites: Grain size and composition dependence, Phys. Earth Planet. Inter., 13, 260, 1977.
Dickson, G. O., C. W. F. Everitt, L. G. Parry, and F. D. Stacey, Origin of thermoremanent magnetization, Earth Planet. Sci. Lett., 1, 222, 1966.
Doell, D. D. and A. Cox, , J. Geophys. Res., 68, 1997, 1963.
Dunlop, D. J., Hysteresis properties of synthetic and natural mono-domain grains. Philos. Mag., 19, 329, 1969.
Dunlop, D. J., Thermoremanent magnetization in submicroscopic magnetite, J. Geophys. Res., 78, 7602–7613, 1973a.
Dunlop, D. J., Superparamagnetic and single-domain threshold sizes in magnetite, J. Geophys. Res., 78, 1780, 1973b.
Dunlop, D. J., Thermal fluctuation analysis; a new technique in rock magnetism, J. Geophys. Res., 81, 3511, 1976.
Dunlop, D. J., The hunting of the ‘Psark’, J. Geomag. Geoelectr., 29, 293–318, 1977.
Dunlop, D. J. and M.-M. Bina, The coercive force spectrum of magnetite at high temperatures: evidence for thermal activation below the blocking temperature, Geophys. J.R. Astron. Soc., 1977 (in press).
Dunlop, D. J. and E. D. Waddington, The field dependence of thermoremanent magnetization of igneous rocks, Earth Planet. Sci. Lett., 25, 11, 1975.
Dunlop, D. J. and G. F. West, An experimental evaluation of single-domain theories, Rev. Geophys., 7, 709, 1969.
Dunlop, D. J., J. A. Hanes, and L. K. Buchan, Indices of multi-domain magnetic behavior in basic igneous rocks: alternating field demagnetization, hysteresis, and oxide petrology, J. Geophys. Res., 78, 1387, 1973.
Dunlop, D. J., F. D. Stacey, and D. E. W. Gillingham, The origin of thermoremanent magnetization: contribution of pseudo single-domain magnetic moments, Earth Planet. Sci. Lett., 21, 288, 1974.
Evans, M. E., Single-domain particles and TRM in rocks, Comments Earth Sci. Geophys., 2, 139,1972.
Evans, M. E. and M. L. Wayman, An investigation of small magnetic particles by means of electron microscopy, Earth Planet. Sci. Lett.,9, 365–370, 1970.
Everitt, C. W. F., Thermoremanent magnetization, I: Experiments on single-domain grains, Philos. Mag., 6, 713, 1961.
Everitt, C. W. F., Thermoremanent magnetization, II: Experiments on multi-domain grains, Philos. Mag., 7, 583, 1962a.
Everitt, C. W. F., Thermoremanent magnetization, III: Theory of multi-domain grains, Philos. Mag., 7, 599, 1962b.
Frei, E. H., S. Shtrikman, and D. Treves, Critical size and nucleation field of ideal ferromagnetic particles, Phys. Rev., 106, 446–455, 1957.
Johnson, H. P., W. Lowrie, and D. V. Kent, Stability of anhysteretic remanent magnetization in fine and coarse magnetite and maghemite particles, Geophys. J.R. Astron. Soc., 41, 1, 1975.
Kittel, C., Physical theory of ferromagnetic domains, Rev. Mod. Phys., 21, 541–583, 1949.
Kneller, E. F. and F. E. Luborsky, Particle size dependence of coercivity and remanence of single- domain particles, J. Appl. Phys., 34, 656, 1963.
Kobayashi, K. and M. D. Fullfr, Stable remanence and memory of multi-domain materials with special reference to magnetite, Philos. Mag., 18, 601, 1968.
Koenigsberger, J. G., Natural residual magnetism of eruptive rocks, Terr. Magn. Atmos. Electr., 43, 119 and 299, 1938.
Kropčàek, V., Self-reversal of spontaneous magnetization of natural cassiterite, Stud. Geophys. Geod. Ceskoslov. Acad. Ved., 19, 108, 1968.
Larson, E., M. Ozima, M. Ozima, T. Nagata, and D. Strangway, Stability of remanent magnetization of igneous rocks, Geophys. J.R. Astron. Soc., 17, 263–292, 1969.
Levi, S., Some magnetic properties of magnetites as a function of grain size and their implications for paleomagnetism, Ph.D. thesis, Univ. of Washington, 1974.
Levi, S. and R. T. Merrill., A comparison of ARM and TRM in magnetite, 1976 (in press).
Levi, S. and R. T. Merrill, Properties of single-domain, pseudo single-domain and multi-domain magnetite, J. Geophys. Res., 1977 (in press).
Lowrie, W., The effects of internal stress on remanence and coercive force in nickel and magnetite, Thesis, University of Pittsburgh, Pittsburgh, Pa., 1967.
Lowrie, W. and M. D. Fuller, On the alternating field demagnetization characteristic of multi- domain magnetization in magnetite, J. Geophys. Res., 76, 6339, 1971.
Luborsky, F. E., Development of elongated fine particle magnets, J. Appl. Phys., 32, 1715, 1901.
Meikeljohn, W. H., Experimental study of the coercive force of fine particles, Rev. Mod. Phys., 25, 302, 1953.
Melloni, M., Napali, Atti. Acc. Sci., 1, 121, 1853.
Merrill, R. T., The demagnetization field of multi-domain magnetite, J. Geomag. Geoelectr., 29, 285–292, 1977.
Morrish, A. H. and S. P. Yu, Dependence of the coercive force on the density of some iron oxide powders, J. Appl. Phys., 26, 1049–1055, 1955.
Murthy, G. S., M. E. Evans, and D. I. Gough, Evidence for single-domain magnetite in the Michikamau anorthosite, Can. J. Earth Sci., 8, 361–370, 1971.
Nagata, T., The mode of causation of thermo-remanent magnetism in igneous rocks, Preliminary note, Bull. Earthq. Res. Inst.,19, 49, 1941, and20, 192, 1942.
Nagata, T., S. Uyeda, and S. Akimoto, Self-reversal of thermoremanent magnetization of igneous rocks, J. Geomag. Geoelectr., 4, 22, 1952.
NéEl, L., Proprietes d’un ferromagnetique cubique en grains fins, C.R. Acad. Sci., 224, 1498, 1947.
NéEl, L., Theorie du trainage magnetique des ferromagnetiques en grains fins avec applications aux terres cuites, Ann. Geophys., 5, 99, 1949.
NéEl, L., Some theoretical aspects of rock magnetism, Adv. Phys., 4, 191, 1955.
Ozima, M. and M. Ozima, Origin of thermoremanent magnetization, J. Geophys. Res., 70, 1363, 1965.
Ozima, M., M. Ozima, and T. Nagata, , J. Geomag. Geoelectr., 16, 37, 1964.
Parry, L. G., Magnetic properties of dispersed magnetite powders, Philos. Mag.,11, 303–311, 1965.
Petrov, I. N. and V. V. Metallova, 12V., Earth Sci., 9, 555, 1968.
Rahman, A. A., A. D. Duncan, and L. G. Parry, Magnetisation of multi-domain magnetite, Riv. Ital. Geofis., 22, 259, 1973.
Rimbert, F., Contribution a l>’etude de Paction de champs alternatifs sur les aimanations remanentes des roches. Applications geophysiques, Rev. Inst. Fr. Pét., 14, 17 and 123, 1959.
Robins, B. W., Remanent magnetization in spinel iron-oxides, Ph.D. thesis, University of New South Wales, Australia, 1972.
Roquet, J., Sur les rémanances magnetiques des oxydes de fer et leur interet en geomagnetisme, Ann. Geophys., 10, 226 and 182, 1954.
Schmidt, V. A., A malti-domain model of thermoremanence, Earth Planet. Sci. Lett., 20, 440–446, 1973.
Schmidt, V. A., The variation of the blocking temperature in models of thermoremanence (TRM), Earth Planet, Sci. Lett., 29, 146, 1976.
Schult, A., Self-reversal of magnetization and chemical composition of titanomagnetites in basalts, Earth Planet. Lett., 4, 440, 1968.
Shive, P. N., Dislocation control of magnetization, J. Geomag. Geoelectr., 21, 519, 1969a.
Shive, P. N., The effect of internal stress on the thermoremanence of nickel, J. Geophys. Res., 74, 381, 1969b.
Soffel, H., The single-domain/multi-domain transition in intermediate titanomagnetites, Z. Geophys., 37, 451, 1971.
Soffel, H., Domain structure of titanomagnetites and its variation with temperature, J. Geomag. Geoelectr., 29, 277–284, 1977.
Stacey, F. D., Thermoremanent magnetization (TRM) of multi-domain grains in igneous rocks, Philos. Mag.,3, 1391, 1958.
Stacey, F. D., A generalized theory of thermoremanence, covering the transition from single-domain to multi-domain magnetic grains., Philos. Mag., 7, 1887, 1962.
Stacey, F. D. and S. K. Banerjee, The Physical Principles of Rock Magnetism, pp. 195, Elsevier, New York, 1974.
Stacey, F. D. and K. N. Wise, Crystal dislocations and coercivity in fine-grained magnetite, Aust. J. Phys., 20, 507, 1967.
Stoner, E. C. and E. P. Wohlfarth, A mechanism of magnetic hysteresis in heterogeneous alloys. Philos. Trans. R. Soc. London, Ser. A, 240, 599–642, 1948.
Syono, Y., S. Akimoto and T. Nagata, Remanent magnetization of ferromagnetic single crystal, J. Geomag. Geoelectr., 14, 113, 1962.
Syono, Y., Magnetocrystalline anisotropy and magnetization of Fe304-Fe2Ti04 series with special application to rock magnetism, Jpn. J. Geophys., 4, 71, 1965.
Thellier, E., Sur l’Aimantations des ferres cuites et ses applications geophysiques, Ann. Inst. Phys. Globe, Univ. Paris,16, 157, 1938.
Uyeda, S., TRM as a medium of paleomagnetism, with special reference to reverse TRM, J. Geomag. Geoelectr., 2, 1, 1958.
Verhoogen, J., The origin of thermoremanent magnetization, J. Geophys. Res., 64, 2441, 1959.
Wasilewski, P. J., Magnetic hysteresis of natural materials, Earth Planet. Sci. Lett., 20, 67, 1973.
Wescott-Lewis, M. F. and L. G. Parry, Thermoremanence in synthetic rhombohedral iron-titanium oxides, Aust. J. Phys., 24, 735, 1971.
Author information
Authors and Affiliations
Editor information
Rights and permissions
Copyright information
© 1977 Center for Academic Publications Japan
About this chapter
Cite this chapter
Day, R. (1977). TRM and Its Variation with Grain Size. In: Dunlop, D.J. (eds) Origin of Thermoremanent Magnetization. Advances in Earth and Planetary Sciences, vol 1. Springer, Dordrecht. https://doi.org/10.1007/978-94-010-1286-7_1
Download citation
DOI: https://doi.org/10.1007/978-94-010-1286-7_1
Publisher Name: Springer, Dordrecht
Print ISBN: 978-94-010-1288-1
Online ISBN: 978-94-010-1286-7
eBook Packages: Springer Book Archive