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Depth versus age based on relative magnetic paleointensity correlations (Fig....
In the figure, the average sedimentation rates are also indicated. The grey bands correspond to the time span of stadial+glacial periods. To the right, the blow-up of the area... -
XRD of Cuttings of the KTB Pilot Hole VB1b
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... -
XRD of Cuttings of the KTB Pilot Hole VB1
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... -
Downhole Resistivity log for HSDP-2-A (environmentally corrected)
The GFZ Potsdam started a log interpretation study in cooperation with the Technical University of Aachen. As a first result, the logged profile allows for a subdivision of the... -
Gas Mass Spectrometry of Gas Samples of the KTB Main Hole HB1a
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... -
Geochemical Analysis of Cations of Mud Samples of the KTB Pilot Hole VB1a.
Geochemical Analysis of Cations of Mud Samples of the KTB Pilot Hole VB1a. -
Radial Vp on Core Samples of the KTB Main Hole HB1g
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 -... -
Geochemical Analysis of Anions of Mud Samples of the KTB Main Hole HB1.
Geochemical Analysis of Anions of Mud Samples of the KTB Main Hole HB1. -
Porosity of Mini Cores (Plugs) of the KTB Pilot Hole VB1
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... -
Relative paleointensity record for CON01-603-2
We established a mastercurve “Baikal 200” of relative paleointensity, which represents a new synthetic paleomagnetic archive for Central Eurasia. The synthetic record is... -
Geochemical Analysis of Anions of Mud Samples of the KTB Pilot Hole VB1a
Geochemical Analysis of Anions of Mud Samples of the KTB Pilot Hole VB1a. -
Gas Mass Spectrometry 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... -
HIRM record for CON01-603-2
We established a mastercurve “Baikal 200” of relative paleointensity, which represents a new synthetic paleomagnetic archive for Central Eurasia. The synthetic record is... -
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... -
Clay mineralogy and sedimentology of coring Site BDP-1-B (BDP93-2)
Lake Baikal, in south-central Siberia, has been the focus of an international effort (the Baikal Drilling Project; BDP) to obtain continuous long cores (upwards of 100 m) from... -
Axial Vs on Core Samples of the KTB Pilot Hole VB1a
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 -... -
Natural Gamma-ray Activity of Cuttings of the KTB Main Hole HB1a (measurement...
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... -
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... -
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... -
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.
