-
Gas chromatography of gas samples of the KTB main hole HB1g
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... -
Gas chromatography of gas samples of the KTB pilot hole VB1b
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... -
Electrical Resistivity of Cores of the KTB Pilot Hole HB1a
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... -
Radial Vp on Core Samples of the KTB Pilot Hole VB1
Ultrasonic wave propagation through core samples is studied in a water tank to insure good signal transmission between transducer, rock specimen and receiver and to avoid time -... -
Permeability of Mini Cores of the KTB Pilot Hole VB1
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.... -
Density of Cuttings 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... -
XRF of Cores 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... -
Biovolume accumulation rates for the dominant planktonic taxa plotted against...
S. grandis is by far the species that contributes the most to the total biovolume accumulation rate with a peak value just above 4×106 μm3 cm−2 year−1. Its relative contribution... -
Downcore variations of SIRM/κLF for VER98-1-14
Higher abundance of greigite during glacial intervals also coincides with small increases of the S content (Fig. 11B). Greigite levels in glacial sediments cannot be correlated... -
Permeability of Mini Cores of the KTB Pilot Hole VB1a: 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.... -
Magnetic Susceptibility of Cuttings of the KTB Pilot Hole HB1h
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... -
The relationship between concentrations of chl-a calculated from SeaWiFS OC2 ...
Values of measured chlorophyll (HPLC=High Pressure Liquid Chromatography) are the mean concentrations of each sampling point from 5 to 30 m depth. For the OC2 chl-a... -
Natural Gamma-ray Activity of Cuttings of the KTB Main Hole HB1h (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... -
Thermal Conductivity of Cores of the KTB Pilot Hole VB1a (measured 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... -
Wet bulk density (GRAPE) of pilot core CONT01-604-3a to piston core CON01-604...
Wet bulk density (GRAPE) of pilot core CONT01-604-3a to piston core CON01-604-3 at Posolskoe -
Magnetic Susceptibility of Cores of the KTB Pilot Hole VB1a
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... -
Thermal Conductivity of Cuttings of the KTB Main Hole HB1a (transformed data)
In the KTB field laboratory, thermal conductivity was measured on cuttings material in depth intervals of 10 m and on available drill core material. The results on drill cores... -
Pedology of the Lake Baikal region
Soil map of the Baikal region from the FAO/IIASA digital soil data base of North and Central Asia (available on CD-ROM). The polygon data were transformed to UTM Z48, WGS 84. *... -
Gas Mass Spectrometry of Gas Samples of the KTB Main Hole HB1i
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... -
Gamma Log for HSDP-2-A on 5. December 1999
The target of this study is to correlate the logging data with the lithological and structural characteristics of the drilled volcanic sequences; in particular to extract...
