Assessing the timing of greigite formation and the reliability of the Upper Olduvai polarity transition record from the Crostolo River, Italy


Roberts, A.P., Jiang, W.T., Florindo, F., Horng, C.S. and Laj, C. (2005) Assessing the timing of greigite formation and the reliability of the Upper Olduvai polarity transition record from the Crostolo River, Italy Geophysical Research Letters, 32, (5), L05307. (doi:10.1029/2004GL022137).

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Description/Abstract

The Crostolo River section in Italy yielded a detailed record of the Upper Olduvai geomagnetic polarity transition that has been used to support the hypothesis of deep mantle control on the transitional geomagnetic field. The paleomagnetic record is carried by the authigenic iron sulphide, greigite, which was interpreted to have formed shortly after deposition. Our detailed scanning electron microscope investigations indicate the presence of at least 3 generations of pyrite, which usually forms with greigite as a precursor. This suggests that the total magnetization is a complex composite that produced a smoothed record of transitional field behaviour.

Item Type: Article
Digital Object Identifier (DOI): doi:10.1029/2004GL022137
ISSNs: 0094-8276 (print)
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ePrint ID: 17408
Date :
Date Event
2005Published
Date Deposited: 07 Sep 2005
Last Modified: 16 Apr 2017 23:15
Further Information:Google Scholar
URI: http://eprints.soton.ac.uk/id/eprint/17408

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