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Detailed Reference Information |
Shcherbakov, V.P., Sycheva, N.K. and Lamash, B.E. (1996). Monte Carlo modelling of TRM and CRM acquisition and comparison of their properties in an ensemble of interacting SD grains. Geophysical Research Letters 23: doi: 10.1029/96GL01999. issn: 0094-8276. |
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Numerical modelling of TRM and of Haigh's model of CRM acquisition was performed using the Monte-Carlo method. It was confirmed that for noninteracting particles, i.e. at small volume concentration c(1--3)%, CRM may be ≥ TRM, though CRM can not exceed TRM more than twice. The relative stability to thermodemagnetisation is always higher for TRM than for CRM. ¿ American Geophysical Union 1996 |
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BACKGROUND DATA FILES |
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Abstract |
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Keywords
Geomagnetism and Paleomagnetism, Rock and mineral magnetism |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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