Research Project
Grant-in-Aid for Challenging Exploratory Research
Magnetic susceptibility of loess-paleosol sediments of the Chinese Loess Plateau reflects the degree of pedogenesis, so that it is often used as a proxy of paleo-rainfall. The magnetic enhancement is caused by pedogenic fine magnetic grains of SP or SD size. This study revealed that SP magnetic grains are concentrated in clastics ranging in size from 1 to 10 μm. Magnetically separated grains consist of abundant silicate minerals that are dominated by muscovite and quite small amount of magnetite grains. We conclude that pedogenic SP magnetic grains exist in silicate minerals as inclusions.
All 2016 2015 Other
All Int'l Joint Research (1 results) Presentation (2 results)