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Reviews of Geophysics, 1983
I have the responsibility of reviewing the advances made in rock magnetism (and paleomagnetic data analysis) over the last four years. My charge includes the specific invitation to comment on the use of rock magnetism in the service of paleomagnetism. This is, of course, a distinction that is often difficult to draw.
Peter N Shive
exaly +2 more sources
I have the responsibility of reviewing the advances made in rock magnetism (and paleomagnetic data analysis) over the last four years. My charge includes the specific invitation to comment on the use of rock magnetism in the service of paleomagnetism. This is, of course, a distinction that is often difficult to draw.
Peter N Shive
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, 1997 Rock Magnetism, first published in 1997, is a comprehensive treatment of fine particle magnetism and the magnetic properties of rocks. Starting from atomic magnetism and magnetostatic principles, the authors explain why domains and micromagnetic structures form in ferromagnetic crystals and how these lead to magnetic memory in the form of thermal ...
David J. Dunlop, Özden Özdemir
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Developments in rock magnetism
Reports on Progress in Physics, 1990Rock magnetism is concerned with the remanent magnetisation of ferrimagnetic fine particles in weak fields ( approximately=0.1 mT), at temperatures ranging from ambient to the Curie point, and over times of geological length. Since most magnetisations in rocks or their synthetic analogues are thermally activated, the blocking temperature below which ...
David J Dunlop
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Introduction to the special section on Fundamental and Frontier Research in Rock Magnetism [PDF]
Journal of Geophysical Research, 2006 Many of the papers in this special section were first presented in the session “Rock Magnetism: Fundamentals and Frontiers” at the 2005 Fall AGU meeting.
Mike Jackson, Wyn Williams
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The Physical Principles of Rock Magnetism
Chemical Geology, 1974 Developments in Solid Earth Geophysics 5: The Physical Principles of Rock Magnetism explores the physical principles of rock magnetism, with emphasis on the properties of finely divided magnetic materials.
Stacey, Frank
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The Moon, 1972
The relationship between the magnetization and temperature in a high constant magnetic field for a temperature range between 5 K and 1100 K was examined for Apollo 11, 12 and 14 lunar materials. The average value of Curie point temperature is (768.2 ± 3.5)°C for the lunar igneous rocks and (762.5 ± 3.4)°C for the lunar fines and breccias.
T. Nagata, R. M. Fisher, F. C. Schwerer
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The relationship between the magnetization and temperature in a high constant magnetic field for a temperature range between 5 K and 1100 K was examined for Apollo 11, 12 and 14 lunar materials. The average value of Curie point temperature is (768.2 ± 3.5)°C for the lunar igneous rocks and (762.5 ± 3.4)°C for the lunar fines and breccias.
T. Nagata, R. M. Fisher, F. C. Schwerer
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Rock Magnetism and the Differentiation of Dolerite Sill
Journal of the Geological Society of Australia, 1954Abstract Measurements of intensity of magnetization and susceptibility have been made at intervals of 5 ft. on some bore cores from Tasmanian tholeiites of Jurassic age. In all cases the direction of magnetization was nearly vertical. One sill appears to have its upper 700 ft. magnetized normally and its lower part reversed.
J. C. Jaeger, Germaine Joplin
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Palaeomagnetism and rock magnetism
Earth-Science Reviews, 1966Summary The magnetic study of rocks leads to three broad fields of knowledge. The first is the history of continental movement as deduced from magnetic rocks, and the comparison of palaeomagnetically determined ancient latitudes with palaeoclimatological evidence. These areas are reviewed quite briefly. The second field is the history of the earth's
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An analysis of rock magnetic data
Proceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences, 1960Abstract The data obtained from numerous palaeomagnetic measurements made during the past decade have shown that while the geologically younger rock formations are magnetized in directions close to that of the present earth’s magnetic field, the remanent magnetic polarizations of older rocks depart markedly from this pattern.
Patrick Maynard Stuart Blackett +2 more
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Exchange Anisotropy in Rock Magnetism
Journal of Applied Physics, 1959Some igneous rocks are magnetized in a direction opposite to that expected, if they had been cooled in the earth's magnetic field. These rocks are said to have a reverse thermo-remanent magnetization (reverse TRM). Uyeda has shown that the reverse TRM of the Haruna deposit in Japan is due to an ilmenite-hematite solid solution and has synthesized a ...
W. H. Meiklejohn, R. E. Carter
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