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Down-core variations of the inclination and declination of ChRM of all invest...
Dashed lines mark some correlation levels of the cores from Lake Baikal with the dated δ18O record from ODP 677 (Shackleton et al., 1990), see also Fig. 3. Diagenetic features... -
XRF of Cores 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... -
High temperature measurement of the saturation magnetisation for VER98-1-14
It shows a loss of a part of the signal at temperatures between 350 and 400 °C, typical disintegration temperatures for greigite. The remaining signal disappears above a... -
Downhole Resistivity log for HSDP-2-A
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... -
XRF of Cuttings of the KTB Main Hole HB1i.
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 ARM for VER 98-1-14
Anhysteretic remanent magnetisation (ARM) measurements, free of the effect of the dia-, para- and superparamagnetic components, provide an estimation of the magnetic remanence... -
Geology of the Lake Baikal region
Geological data sets of the Baikal region based on the USGS digital data of Asian petroleum provinces. The attributation of polygon data was partly reassigned and the maps... -
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... -
Natural Remanent Magnetisation of Cores of the KTB Main Hole HB1
Natural Remanent Magnetisation of Cores of the KTB Main Hole HB1 -
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... -
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. *... -
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... -
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... -
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... -
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... -
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... -
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.... -
SAFOD Main Hole downhole logging data phase 1.2 2124-2353m, year: 2004
SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major... -
Natural Gamma-ray Activity of Cores of the KTB Main Hole HB1g
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... -
XRD of Cores of the KTB Main Hole HB1g
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...