210 datasets found

Laboratory processing of concentrates was aimed at the removal of non-sporomorph organic matter by means of chemical treatment, micro-sieving and heavy liquid seperation. The...

Geochemical Analysis of Anions of Mud Samples of the KTB Main Hole HB1h.

Catchment areas of Lake Baikal catchment, projected in UTM Z48, WGS 84. The data were taken from Swiercz, S. (2004). GIS supported characterization of the Baikal region. Diploma...

Infrastructure data sets of the Lake Baikal region based on the Digital Chart of the World (DCW). DCW data of southern Siberia, norther Mongolia,north-west China merged and...

SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major...

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...

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 -...

Supplementary material to B. Heim et al. (2008): Assembly and concept of a web-based GIS within the paleoclimate project CONTINENT (Lake Baikal, Siberia)

High temperature measurements of magnetic susceptibility in clay-rich layers. Magnetite, characterised by a Curie temperature of 590 °C, dominates the signal.

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...

The vertical distribution of organisms in the sediment indicates that animals can be present as deep as 15 cm although at very low abundance at such depths (Fig. 4, Fig. 5 and...

Geochemical Analysis of Anions of Mud Samples of the KTB Pilot Hole VB1.

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...

Geochemical Analysis of Anions of Mud Samples of the KTB Main Hole HB1g.

High temperature measurements of magnetic susceptibility in diatomaceous layers. Most of the weak susceptibility is still present up to the temperature of 670 °C and carried by...

Vegetation map of the Baikal region, edited by J. Klump, B. Heim and S. Schneider. The map is based on: Isachenko, T. I. (1990): Vegetation of the USSR. Government...

Geochemical Analysis of Cations of Mud Samples of the KTB Pilot Hole VB1b.

The day plot (Fig. 6B; Day et al., 1977) indicates that samples with S-ratios >0.95 plot rather in the single-domain (SD) to pseudosingle-domain (PSD) range. Samples with...

Porewater samples were conserved with 0.2% chloroform and analyzed at EAWAG, Switzerland, for NO3-, NH4+, SiO2, and o-PO4 using standard photometric methods (DEW, 1996). In...

Geochemical Analysis of Anions Of Mud Samples of the Ktb Main Hole HB1d.