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Depth versus age based on relative magnetic paleointensity correlations (Fig....
In the figure, the average sedimentation rates are also indicated. The grey bands correspond to the time span of stadial+glacial periods. To the right, the blow-up of the area... -
Geochemistry of sediment core BDP-2-A ( BDP96-1) from Lake Baikal
Geochemistry of sediment core BDP-2-A ( BDP96-1) from Lake Baikal -
Magnetic Susceptibility of Mini-Cores of the KTB Main Hole HB1
The magnetic susceptibility is measured by an inductive AC device (BARTINGTON). The sample is placed inside a coil which generates an alternating magnetic field. The applied... -
Diatom record (in relative percentages) and the biovolume accumulation rates ...
The diatom succession at Academician Ridge is similar to the one from Continent Ridge and the two records, despite having very different sampling resolution, can be easily... -
Density of Cuttings of the KTB Main Hole HB1i
The density of rocks depends on the mineral contents and is therefore a helpful property for the discrimination of lithological units. It is also used for the calculation of... -
Thermal Conductivity of Cores of the KTB Pilot Hole VB1 (transformed data)
The thermal conductivity on cores is measured in two steps (see Pribnow 1994). First, one face end of the core is sawed and polished. The half space line source is pressed... -
XRD of Cores of the KTB Main Hole HB1d
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... -
Downcore variations of the water content for the sedimentary sequence of VER ...
The water content was determined from samples retrieved with cylindrical syringe samplers, weighed wet and weighed again after freeze-drying. The clay-rich layers are... -
Magnetic Susceptibility of Mini-Cores (Plugs) of the KTB Pilot Hole VB1
The magnetic susceptibility is measured by an inductive AC device (BARTINGTON). The sample is placed inside a coil which generates an alternating magnetic field. The applied... -
Depth versus age based on relative magnetic paleointensity correlations for a...
In order to characterise Lake Baikal sedimentary responses to global climatic changes that may be recorded in marine sediments, we compared our paleomagnetically dated... -
SAFOD Main Hole downhole logging data phase 1.2 1368-1556m
SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major... -
Wet bulk density of core CON01-605-3a, the trigger core to piston core CON01-...
Wet bulk density of core CON01-605-3a, the trigger core to piston core CON01-605-3 at Vydrino -
Natural Gamma-ray Activity of Cuttings of the KTB Main Hole HB1d (measurement...
In the laboratory, the gamma radiation is measured by a sodium iodtite (NaI) scintillation detector (cores and cuttings) and by a germanium (Ge) semiconductor detector... -
Raw pollen data from the Eemian core CON01-603-2
The studied core CON01-603-2 was recovered from the Continent site, Northern Basin from a water depth of 386 m (Fig. 1) (see Charlet et al., 2005-this volume). The analysed... -
Porosity of Mini Cores (Plugs) of the KTB Main Hole HB1i
Therefore, at room temperature and under vacuum the samples were submerged in destilled water for at least 24 hours. Afterwards atmospheric pressure was applied for at least 24... -
Permeability of Mini Cores of the KTB Pilot Hole VB1: Instationary Measurements
In the KTB field laboratory, porosity, internal surface and permeability were determined on identical mini cores with 25.4 mm in diameter and approximately 50 mm in length.... -
Major composition (wt.%) of concretions, ICP-AES measurements
In order to get a complete geochemical signature, 14 P-rich concretions, chosen among the different cores, were acid digested (Table 3a and Table 3b). In a clean laboratory, 1.7... -
Thermal Conductivity of Cores of the KTB Pilot Hole VB1a (transformed data)
The thermal conductivity on cores is measured in two steps (see Pribnow 1994). First, one face end of the core is sawed and polished. The half space line source is pressed... -
Gas Radon Measurements of Gas Samples of the KTB Main Hole HB1
In the complete KTB-VB and in in the KTB-HB down to a depth of 3003 m the gas phase was released and collected by twirl degassers attached in front of the mud shakers. This open... -
Density of Cuttings of the KTB Pilot Hole Vb1
The density of rocks depends on the mineral contents and is therefore a helpful property for the discrimination of lithological units. It is also used for the calculation of...
