210 datasets found

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...

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...

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...

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...

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...

Inland waters of the Baikal region based on the Digital Chart of the World (DCW). DCW data of southern Siberia, northern Mongolia, north-west China merged into one map 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...

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

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

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...

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...

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

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...

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...

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

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 Pilot Hole VB1.

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...