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Age models based on palaeomagnetic measurements for the two cores analysed, C...
Palaeomagnetism was the method used for dating sediments older than the time span covered by AMS 14C dating. Geomagnetic palaeointensities recorded in Lake Baikal sediments were... -
Gas Radon Measurements of Gas Samples of the KTB Main Hole HB1g
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 Cuttings of the KTB Main Hole HB1d
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... -
Gas chromatography of gas samples of the KTB main hole HB1d
The main objective of this drilling fluid analysis was the detection of inflows of formation fluids. Therefore different gases dissolved in the drilling mud were measured... -
Natural Gamma-ray Activity of Cuttings of the KTB Pilot Hole VB1a
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... -
XRF of Cores of the KTB Main Hole KTB-HB1.
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 water content for the sedimentary sequence of VER ...
The water content was determined from samples retrieved with cylindrical syringe samplers, weighed wet and weighed again after freeze-drying. The clay-rich layers are... -
Borehole Temperature of HSDP-2-A on 04/19/1999
The temperature pattern is attributed to a superposition of thermal and hydraulic processes. In the deeper borehole (HSDP-2, depth 3.1 km) detailed temperature monitoring was... -
Depth profiles of marker pigments from Bacillariophyceae plus Chrysophyceae (...
The traps were deployed for about 16 months. The respective regression equations and its coefficients of determination (r2) are reported in Table 5.In the 40-m trap, fucoxanthin... -
Water content and dry bulk density of pilot core CON01-605-3a to piston core ...
Water content and dry bulk density of pilot core CON01-605-3a to piston core CON01-605-3 at Vydrino -
XRD of Cuttings of the KTB Main Hole HB1h
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... -
Geochemistry of sediment core BDP-2-A ( BDP96-1) from Lake Baikal
Geochemistry of sediment core BDP-2-A ( BDP96-1) from Lake Baikal -
Trace element composition of concretions, ICP–MS measurements
In order to get a complete geochemical signature, 14 P-rich concretions, chosen among the different cores, were acid digested (Table 3a and Table 3b). In a clean laboratory, 1.7... -
Magnetic Susceptibility of Mini-Cores of the KTB Main Hole HB1g
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... -
Gas Radon Measurements of Gas Samples of the KTB Main Hole HB1d
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... -
Diatom valve concentration in wet sediment, diatom frustule accumulation rate...
At both sites, the lowest dry bulk density values (ca. 0.40 g cm−3) correspond to intervals with high diatom concentrations and high sediment accumulation rate. By contrast, the... -
Water content and dry bulk density of piston core CON01-603-2 from CONTINENT ...
Water content and dry bulk density of piston core CON01-603-2 from CONTINENT Ridge -
High temperature measurements of magnetic susceptibility in clay-rich layers
High temperature measurements of magnetic susceptibility in clay-rich layers. Magnetite, characterised by a Curie temperature of 590 °C, dominates the signal. -
δ13C(organic), C/N mass ratios and %TOC for Continent Ridge core CON01-603-5
C/N mass ratios remain constant throughout MIS 3 and into MIS 2, with values between 6.3 and 8.9, indicating no significant terrestrial input of organic matter (Fig. 3). Low... -
XRF of Cuttings 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...