The magnetic properties of siderite concretions and the CRM of their oxidation products

Details The magnetic properties of siderite concretions and the CRM of their oxidation products The magnetic properties of siderite concretions and the CRM of their oxidation products

Oct 1990

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1990pepi...63...41h&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 63, Issue 1-2, p. 41-57.

Physics

5

Scientific paper

Siderite concretions found in the perimarine Pleistocene sediments of the Campine Formation in northeast Belgium have a stable natural remanent magnetization which can be mainly attributed to magnetic carriers locked in during their growth. Room-temperature oxidation of the concretions resulted mainly in hematite which acquires a field-controlled, very stable crystalline remanent magnetization. Siderite samples heated in air did not show magnetic interactions between the dissociation products hematite and maghemite.

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