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Gas Radon Measurements 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... -
XRD of Cuttings of the KTB Pilot Hole VB1a
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... -
XRF of Centrifuge Samples of the KTB Pilot Hole VB1a.
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 relative sulphur content, estimated by XRF counting, ...
Increased presence of greigite (high SIRM/κLF) coincides with maximum sulphur contents observed at the beginning of interglacial stages (Fig. 11A). At similar levels in another... -
Density of Core Samples of the KTB Main Hole HB1
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... -
Densities of benthic taxa with depth (CON 01-01 and CON 01-04 expeditions).
In all abyssal stations, densities are never over an average of c. 3100 individuals m−2 (Fig. 3, Table 1). In contrast, the shallow station (CON01-427, Posolskoe Bank) harbours... -
Gas mass spectrometry of gas samples from the KTB Main Hole HB1
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... -
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... -
Permeability of Mini Cores of the KTB Main Hole HB1g
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.... -
Magnetic Susceptibility of Cuttings of the KTB Pilot Hole HB1d
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... -
Wet bulk density of pilot core to CON01-603-2 (CONTINENT Ridge) measured by G...
Wet bulk density of pilot core to CON01-603-2 (CONTINENT Ridge) measured by GRAPE density -
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.... -
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... -
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... -
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... -
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... -
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 -
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...