Normalized magnetic parameters and their applicability to paleomagnetism and environmental magnetism

Publisher Website
Google Scholar
Abstract
Using simple theory, one can show that normalized magnetic parameters—i.e., one primary magnetic measurement divided by a second—are not independent of the concentration of magnetic minerals in an assemblage, except in a few special cases. In the common situation, when the number of minerals in an assemblage is unknown, these parameters can only be used to show a lack of change in domain size or mineralogy.

This publication has 0 references indexed in Scilit: