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SAFOD Main Hole downhole logging data phase 1.2 1744-1932m
SAFOD
2008
SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major plate-bounding fault. SAFOD will drill and instrument an inclined borehole across the San Andreas Fault Zone to a depth of 3.2...
SAFOD Main Hole downhole logging data phase 1.2 1932-2041m
SAFOD
2008
SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major plate-bounding fault. SAFOD will drill and instrument an inclined borehole across the San Andreas Fault Zone to a depth of 3.2...
SAFOD borehole trajectory data in absolute coordinates (UTM) and in coordinates relative to drilling platform
SAFOD
2007
SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major plate-bounding fault. SAFOD will drill and instrument an inclined borehole across the San Andreas Fault Zone to a depth of 3.2...
SAFOD Main Hole downhole logging data phase 1.1
SAFOD
2007
SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major plate-bounding fault. SAFOD will drill and instrument an inclined borehole across the San Andreas Fault Zone to a depth of 3.2...
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 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 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...
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...