Abstract
This is the first of four chapters devoted to the techniques for collecting and analysing kinematic data. The fundamental source of data for determining past plate motions is furnished by rock magnetization. In this chapter, I describe the different classes of rock magnetism, the main magnetic minerals, and the origin of ferromagnetism.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
References
Butler RF (1992) Paleomagnetism: magnetic domains to Geologic terranes. Blackwell Scientific Publications, Boston, p 238
de Boer CB, Mullender TAT, Dekkers MJ (2001) Low-temperature behaviour of haematite: susceptibility and magnetization increase on cycling through the Morin transition. Geophys J Int 146:201–16
Feynman RP, Leighton RB, Sands M (2006) The Feynman lectures on physics, The definitive edition, vol 2, Chapter 34. Pearson Education Inc., California Institute of Technology, Pasadena, CA
Harrison RJ, Putnis A (1996) Magnetic properties of the magnetite-spinel solid solution: curie temperatures, magnetic susceptibilities, and cation ordering. Am Miner 81:375–84
Hunt CP, Moskowitz BM, Banerjee SK (1995) Magnetic properties of rocks and minerals. In: Ahrens TJ (ed) Rock physics and phase relations: a handbook of physical constants, 3rd edn. AGU, Washington, DC, pp 189–204. doi:10.1029/RF003p0189
Panofsky WKH, Phillips M (2005) Classical electricity and magnetism. Courier Dover, Mineola, NY
Author information
Authors and Affiliations
Rights and permissions
Copyright information
© 2015 Springer International Publishing Switzerland
About this chapter
Cite this chapter
Schettino, A. (2015). Magnetization and Magnetic Minerals. In: Quantitative Plate Tectonics. Springer, Cham. https://doi.org/10.1007/978-3-319-09135-8_3
Download citation
DOI: https://doi.org/10.1007/978-3-319-09135-8_3
Published:
Publisher Name: Springer, Cham
Print ISBN: 978-3-319-09134-1
Online ISBN: 978-3-319-09135-8
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)