Origin of maghaemite in Chinese loess deposits: aeolian or pedogenic?
- 16 April 1999
- journal article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 112 (3-4), 191-201
- https://doi.org/10.1016/s0031-9201(99)00002-3
Abstract
No abstract availableKeywords
This publication has 35 references indexed in Scilit:
- Rock MagnetismPublished by Cambridge University Press (CUP) ,1997
- Mössbauer spectroscopy analysis of iron‐containing minerals in the Chinese loessJournal of Geophysical Research, 1995
- Loess magnetismReviews of Geophysics, 1995
- Magnetic Enhancement of Chinese Loess-The Role of γFe2O3?Geophysical Journal International, 1994
- Magnetic Enhancement and Palaeoclimate: Study of A Loess/Palaeosol Couplet Across the Loess Plateau of ChinaGeophysical Journal International, 1994
- Size-induced structural phase transitions and hyperfine properties of microcrystalline Fe2O3Journal of Physics C: Solid State Physics, 1988
- Palaeoclimatic and sedimentary history from magnetic susceptibility of loess in ChinaGeophysical Research Letters, 1986
- Magnetism of Chinese loess depositsGeophysical Journal International, 1984
- Magnetostratigraphical dating of loess deposits in ChinaNature, 1982
- The Effect of Particle Size of γ-Fe2O3 on the Transformation from γ-Form to α-FormJapanese Journal of Applied Physics, 1965