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3130 data publications found
Depth versus age based on relative magnetic paleointensity correlations for all six investigated sites
Demory, Francois | Nowaczyk, Norbert | Witt, Annette | Oberhänsli, Hedi
2006
In order to characterise Lake Baikal sedimentary responses to global climatic changes that may be recorded in marine sediments, we compared our paleomagnetically dated climate-proxy record from Lake Baikal with benthic and plankontic δ18O curves of ODP Site 983, a site close to ODP Site 984....
Down-core variations of normalised relative paleointensity after removal of intervals affected by diagenesis
Demory, Francois | Nowaczyk, Norbert | Witt, Annette | Oberhänsli, Hedi
2006
Down-core variations of normalised relative paleointensity after removal of intervals affected by diagenesis (magnetite dissolution and/or greigite formation) and correlation to the relative paleointensity record from ODP Site 984 (Channell, 1999). In addition to AMS 14C dating and 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...
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...
Vector endpoint data for CON01-603-2.
Demory, Francois | Nowaczyk, Norbert | Witt, Annette | Oberhänsli, Hedi
2006
Three representative vector endpoint diagrams: (A) sample from a clay-rich layer, exhibiting normal polarity; (B) sample from a clay-rich layer, exhibiting reverse polarity, with the separation of the stable remanence after removal of the normal viscous overprint; (C) instable remanence of a...
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...
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...
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 HB1a
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...