Article ID Journal Published Year Pages File Type
1041968 Quaternary International 2014 12 Pages PDF
Abstract
The magnetic mineralogy of the pilot samples is determined by isothermal remanent magnetisation (IRM) measurements. No differences between loess samples with different sedimentary structure could be shown. The dominant phase in the magnetic fabric that determined the magnetic character of samples was magnetite/maghemite.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geology
Preview
Quaternary surface processes indicated by the magnetic fabric of undisturbed, reworked and fine-layered loess in Hungary
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