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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... -
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 -... -
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... -
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... -
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... -
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... -
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... -
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... -
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...
