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XRD of Cuttings of the KTB Pilot 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 Cuttings of the KTB Pilot Hole HB1i
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... -
Down-core variations of normalised relative paleointensity and ARM/SIRM after...
The concentration in ferromagnetic particles is much lower in the interglacial sediments than in glacial sediments. Therefore, the NRM needs to be normalised by a... -
Diatom concentration for Continent Ridge core CON01-603-5
All diatoms in the analysed section were extensively affected by dissolution with only c. 1% of valves in a “pristine” condition. Diatom concentrations were generally extremely... -
SAFOD Main Hole downhole logging data phase 1.2 1932-2041m
SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major... -
XRF of Cores of the KTB Main Hole HB1d.
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... -
Pollen counts from Kasten corer CON01-603-5, CONTINENT Ridge
Pollen counts from Kasten corer CON01-603-5 at CONTINENT Ridge. -
Porosity of Mini Cores (Plugs) of the KTB Main Hole HB1a
The porosity was determined using the most common Archimedian method (Schopper, 1982). It is based on the following three weight determinations of the sample: (1) The samples... -
Axial 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 -... -
Density of Core Samples 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... -
XRF of Cores of the KTB Main Hole HB1a.
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... -
XRF titanium, iron counting and ratio Fe/Ti for CON01-603-2 and VER98-1-14
In selected intervals, we measured titanium and iron contents in parallel to rock magnetic parameters (Fig. 9). Titanium content is a good reflection of detrital input since... -
Gas Radon Measurements 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... -
Dry bulk density and water content of piston core CON01-605-3 from Vydrino
Dry bulk density and water content of piston core CON01-605-3 from Vydrino -
Bathymetry of Lake Baikal
The bathymetric data were derived from "A bathymetric map of Lake Baikal" (Marc de Batist et al., 2002, doi:10.1595/GFZ.SDDB.1100 ).The map of de Batist et al. is based on all... -
Lithological map of the Lake Baikal catchment
Lithology of the Lake Baikal catchment area, based on a USGS geological data set (http://energy.cr.usgs.gov/oilgas/wep/products/geology/fsu.htm) and edited according to Russian... -
Natural Gamma-ray Activity of Cuttings of the KTB Main Hole HB1g (measuremen...
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... -
Geochemistry of sediment core BDP-1-A (BDP93-1)
Major and trace elements in the 100 m drilling core samples from Lake Baikal have been determined by ICP-AES (inductively coupled plasma atomic emission spectrometry), ICP-MS... -
Hysteresis measurements (uncorrected and corrected for the paramagnetic influ...
Hysteresis measurements of a greigite dominated clay -rich layer with single-domain behaviour hysteresis loop for VER98-1-1. -
Selected electron-microprobe analyses of vivianite and santabarbaraite from L...
Electron-microprobe analyses (Table 5) were completed on a selection of grains from 11 samples, with a CAMECA SX-50 instrument (University of Louvain-la-Neuve, Belgium), under...
