Abstract
A prior knowledge of the domain states and composition of the magnetic grains in basalts could be helpful in planning palaeointensity investigations and this could be obtained by simple techniques. The behaviour of basalt samples containing different types of magnetic grains on heating and cooling is presented and the feasibility of estimating palaeointensity from such samples is discussed.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
