A comparison of the magnetization of detrital and chemical sediments from Lake Zurich | Zendy

Giovanoli Federico | Zendy

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A comparison of the magnetization of detrital and chemical sediments from Lake Zurich

Author(s) -

Giovanoli Federico

Publication year - 1979

Publication title -

geophysical research letters

Language(s) - English

Resource type - Journals

SCImago Journal Rank - 2.007

H-Index - 273

eISSN - 1944-8007

pISSN - 0094-8276

DOI - 10.1029/gl006i004p00233

Subject(s) - remanence , magnetization , silt , geology , natural remanent magnetization , glacial period , rock magnetism , paleomagnetism , clockwise , yield (engineering) , magnetostratigraphy , mineralogy , geochemistry , geophysics , geomorphology , materials science , magnetic field , physics , metallurgy , quantum mechanics , amplitude

Glacial clay and silt rhythmites retain a stable remanent magnetization. Their remanence directions yield a clockwise loop with a periodicity of about 400 years. When diagenetically formed iron sulphides are present, then the magnetization direction curves are not correlatable.

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