High temperature measurements of magnetic susceptibility in clay-rich layers for VER98-1-14

Cite as:

Demory, Francois; Oberhänsli, Hedi; Nowaczyk, Norbert; Gottschalk, Matthias; Wirth, Richard; Naumann, Rudolf (2006): High temperature measurements of magnetic susceptibility in clay-rich layers for VER98-1-14. Deutsches GeoForschungsZentrum GFZ. https://doi.org/10.1594/GFZ.SDDB.1025

Status

I N R E V I E W : Demory, Francois; Oberhänsli, Hedi; Nowaczyk, Norbert; Gottschalk, Matthias; Wirth, Richard; Naumann, Rudolf (2006): High temperature measurements of magnetic susceptibility in clay-rich layers for VER98-1-14. Deutsches GeoForschungsZentrum GFZ. https://doi.org/10.1594/GFZ.SDDB.1025

Abstract

High temperature measurements of magnetic susceptibility in clay-rich layers. Magnetite, characterised by a Curie temperature of 590 °C, dominates the signal.

Authors

Demory, Francois
Oberhänsli, Hedi
Nowaczyk, Norbert
Gottschalk, Matthias
Wirth, Richard
Naumann, Rudolf

Keywords

, Geology

GCMD Science Keywords

EARTH SCIENCE > Paleoclimate > Ocean/Lake Records > Paleomagnetic Data

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