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

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

2006

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

High temperature measurements of magnetic susceptibility in clay-rich layers

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

2006

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

High temperature measurements of magnetic susceptibility in diatomaceous layers for VER98-1-1

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

2006

High temperature measurements of magnetic susceptibility in diatomaceous layers. Most of the weak susceptibility is still present up to the temperature of 670 °C and carried by hematite.

Related materials to Lauterbach et al. (2011) Environmental responses to Lateglacial climatic fluctuations recorded in the sediments of pre-Alpine Lake Mondsee (northeastern Alps)

Lauterbach, Stefan | Brauer, Achim | Andersen, Nils | Danielopol, Dan | Dulski, Peter | Hüls, Matthias | Milecka, Krystyna | Namiotko, Tadeusz | Obremska, Milena | von Grafenstein, Ulrich

2011

Investigation of the sedimentary record of pre-Alpine Lake Mondsee (Upper Austria) focused on the environmental reaction to rapid Lateglacial climatic changes. Results of this study reveal complex proxy responses that are variable in time and influenced by the long-term evolution of the lake...

Supplementary material to Lauterbach et al. (2010): Multi-proxy evidence for early to mid-Holocene environmental and climatic changes in northeastern Poland

Lauterbach, S | Brauer, A. | Andersen, N. | Danielopol, D.L. | Dulski, P. | Hüls, M. | Milecka, K. | Namiotko, T. | Plessen, B. | von Grafenstein, U. | Participants DECLAKES

2010

We investigated the sedimentary record of Lake Hancza (northeastern Poland) using a multi-proxy approach, focusing on early to mid-Holocene climatic and environmental changes. AMS 14C dating of terrestrial macrofossils and sedimentation rate estimates from occasional varve thickness...

Down-core variations of normalised relative paleointensity and ARM/SIRM after diagenetic correction for CON01-603-2.

Demory, Francois | Nowaczyk, Norbert | Witt, Annette | Oberhänsli, Hedi

2006

The concentration in ferromagnetic particles is much lower in the interglacial sediments than in glacial sediments. Therefore, the NRM needs to be normalised by a concentration-related parameter, such as κLF, ARM or SIRM, in order to generate relative paleointensity records free of the...

Down-core variations of the SIRM for CON01-603-2.

Demory, Francois | Nowaczyk, Norbert | Witt, Annette | Oberhänsli, Hedi

2006

The concentration in ferromagnetic particles is much lower in the interglacial sediments than in glacial sediments. Therefore, the NRM needs to be normalised by a concentration-related parameter, such as κLF, ARM or SIRM, in order to generate relative paleointensity records free of the...

XRD of Cuttings of the KTB Main Hole HB1i

KTB, WG Geochemistry

2010

The qualitative and quantitative phase analyses were performed in the KTB field laboratory by x-ray powder diffraction using SIEMENS D 500 diffractometer. During early stages of the KTB project a new method for quantitative phase analysis was developed (see references below). The method is...

XRD of Cores of the KTB Main Hole HB1g

KTB, WG Geochemistry

2010

The qualitative and quantitative phase analyses were performed in the KTB field laboratory by x-ray powder diffraction using SIEMENS D 500 diffractometer. During early stages of the KTB project a new method for quantitative phase analysis was developed (see references below). The method is...

XRD of Cores of the KTB Main Hole HB1i

KTB, WG Geochemistry

2010

The qualitative and quantitative phase analyses were performed in the KTB field laboratory by x-ray powder diffraction using SIEMENS D 500 diffractometer. During early stages of the KTB project a new method for quantitative phase analysis was developed (see references below). The method is...