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Magnetic properties of the Old Crow tephra: Identification of a complex iron titanium oxide mineralogy

The mineralogy and grain‐size distribution of the Fe‐Ti oxide population of the Old Crow tephra bed, outcropping at the Halfway House loess deposit in central Alaska, are characterized through multiple low‐ and high‐temperature magnetization experiments. The characterization is facilitated by heavy...

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Bibliographic Details
Published in:Journal of Geophysical Research: Solid Earth 2004-01, Vol.109 (B1), p.B01104.1-n/a
Main Authors: Lagroix, France, Banerjee, Subir K., Jackson, Mike J.
Format: Article
Language:English
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Summary:The mineralogy and grain‐size distribution of the Fe‐Ti oxide population of the Old Crow tephra bed, outcropping at the Halfway House loess deposit in central Alaska, are characterized through multiple low‐ and high‐temperature magnetization experiments. The characterization is facilitated by heavy liquid separation of the bulk sample into a low‐density ( 0.8 and may play an equally important role as magnetic indicator of titanomagnetite. Furthermore, we demonstrate the ability of low‐temperature magnetism to locate a 1 mm thick tephra bed dispersed in loess over 10 cm depth, through the identification of very low concentrations of a titanohematite phase with y = 0.9. The potential for advancing regional correlation of sedimentary deposits through the identification of Fe‐Ti oxides common to tephra beds by low‐temperature magnetism is illustrated in this study.
ISSN:0148-0227
2169-9313
2156-2202
2169-9356
DOI:10.1029/2003JB002678