COMPARISON OF THE MAGNETIZATION OF DETRITAL AND CHEMICAL SEDIMENTS FROM LAKE ZURICH

被引：11

作者：

GIOVANOLI, F

机构：

来源：

GEOPHYSICAL RESEARCH LETTERS | 1979年 / 6卷 / 04期

关键词：

D O I：

10.1029/GL006i004p00233

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

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. Copyright 1979 by the American Geophysical Union.

引用

页码：233 / 235

页数：3

共 7 条

[1]

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[2]

Kelts K., 1978, THESIS ETH ZURICH

[3]

Rickard D., 1969, STOCK CONTRIB GEOL, V20, P67

[4] MAGNETIC PROPERTIES AND MOSSBAUER-SPECTRA OF SYNTHETIC SAMPLES OF FE3S4 [J].