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Magnetic field downlog 19990704 for HSDP-2-A
A quasi-continuous magnetic log has been obtained in the Hawaii Scientific Drilling Project 2 (HSDP-2) between 600 m and 1800 m, which corresponds to a time interval of... -
Downcore variations of the S-ratio for CON01-603-2, CON01-604-2, CON01-605-3,...
In interglacial sediments, the magnetic assemblages depict changes in the sedimentation rate, which are traced using the ratio of magnetite over hematite (S-ratio). At the... -
Unit-cell parameters and Mn(Fe+Mn) ratios of vivianites from Lake Baikal
The unit-cell parameters (Table 4) were calculated with the least-squares refinement program LCLSQ 8.4 (Burnham, 1991), from the d-spacings corrected with an internal standard... -
Vertical distribution in the sediment of the different animal groups found in...
The vertical distribution of organisms in the sediment indicates that animals can be present as deep as 15 cm although at very low abundance at such depths (Fig. 4, Fig. 5 and... -
Composition of major oxide in bulk sediments from lake Baikal: ICP-AES data f...
The sediment cores were sampled with a resolution of 10 cm, resulting in a total of 290 samples (Table 2). Around 250 mg of dried sediments was mechanically crushed through... -
SAFOD Main Hole downhole logging data phase 1.2 1744-1932m
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 HB1a
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... -
Depth profiles of the contribution to total chlorophyll a+chlorophyllide a by...
Calculations were based on factors established for 89 water samples across Lake Baikal in July 2001 (see text). The traps were deployed for about 16 months and the core top... -
Relative percentage diatom profile for BAIK38 (BAIK94-38A), using uncorrected...
Fig. 3 is the diatom stratigraphy of dominant phytoplankton taxa for BAIK38 expressed as relative percentages, plotted against the age scale. Zone 1 (c. 880 AD–c. 1180 AD) is... -
Gas chromatography of gas samples of the KTB pilot hole VB!
The main objective of this drilling fluid analysis was the detection of inflows of formation fluids. Therefore different gases dissolved in the drilling mud were measured... -
%dry weight and %loss on ignition for CON01-603-5
%dry weight and %loss on ignition for CON01-603-5 -
Natural Remanent Magnetisation of Cores of the KTB Main Hole HB1a
Natural Remanent Magnetisation of Cores of the KTB Main Hole HB1a -
Wet bulk density of core CON01-603-4a, the trigger core to piston core CON01-...
Wet bulk density of core CON01-603-4a, the trigger core to piston core CON01-603-4 at CONTINENT Ridge -
Paleointensity versus age of all the sedimentary sequences of the present study
Paleointensity versus age of all the sedimentary sequences of the present study, of the synthetic curve resulting from its compilation from other curves, and of the reference... -
Density of Core Samples of the KTB Main Hole HB1a
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... -
Electrical Resistivity of Mini Cores (Plugs) of the KTB Main Hole HB1
In general, four-electrode devices are used to measure the resistivity on original (unprepared) cores and on mini cores drilled from these original cores. The in-phase and the... -
XRF of Cuttings 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... -
Downcore variations of the opal content for the sedimentary sequence of VER98...
Opal content was obtained by measuring the NaCO3 leached solution by inductive coupled plasma with an optical emission spectrometer (ICP-OES). The clay-rich layers are... -
Relative percentage diatom profile for BAIK94-38A using corrected values for ...
Preservation differences can be used as correction factors to recalculate the relative abundances of each of the five dominant plankton taxa in BAIK38 and are depicted in Fig.... -
Magnetic Susceptibility of Cuttings of the KTB Pilot Hole HB1a
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...