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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 -
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... -
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... -
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... -
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... -
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... -
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... -
X-ray Computed Tomography and borehole televiewer images of the Alpine Fault’...
The orientations and densities of fractures in the foliated hanging-wall of the Alpine Fault provide insights into the role of a mechanical anisotropy in upper crustal... -
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... -
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... -
Geochemistry of sediment core BDP-2-A ( BDP96-1) from Lake Baikal
Geochemistry of sediment core BDP-2-A ( BDP96-1) from Lake Baikal -
XRF of Centrifuge Samples of the KTB Pilot Hole VB1.
Cuttings were crushed in a tungsten carbide ball mill for 25 min; while core samples were crushed in a tungsten carbide jaw breaker and then processed in the same way as the... -
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... -
AMS radiocarbon dates of pollen from Lake Baikal sediments
AMS radiocarbon dates of pollen from Lake Baikal sediments -
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... -
XRD of Cuttings of the KTB Pilot Hole VB1b
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... -
XRD of Cuttings of the KTB Pilot Hole VB1
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... -
Downhole Resistivity log for HSDP-2-A (environmentally corrected)
The GFZ Potsdam started a log interpretation study in cooperation with the Technical University of Aachen. As a first result, the logged profile allows for a subdivision of the... -
Natural Gamma-ray Activity of Cores of the KTB Pilot Hole VB1a
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... -
Gas Mass Spectrometry of Gas Samples of the KTB Main Hole HB1h
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...
