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Infrared-Spectrometry on Cutting Samples of the KTB Main Hole (Drill Section ...
Infrared-Spectrometry on Cutting Samples of the KTB Main Hole (Drill Section HB1g), 7220-8322 m. -
Raw pollen data from kasten core CON01-603-5 part2 (counts)
Sediment slices of 0.5 cm thickness were obtained from gravity core segments and of 1 cm thickness from the Vydrino piston core. Volumetric subsamples of 5 cm3 (10 cm3 in case... -
Thermal Conductivity of Cuttings of the KTB Main Hole HB1g (transformed data)
In the KTB field laboratory, thermal conductivity was measured on cuttings material in depth intervals of 10 m and on available drill core material. The results on drill cores... -
Intercorrelation of down-core variations of the high-resolution magnetic susc...
Down-core variations of the high-resolution magnetic susceptibility (0.1 cm steps)have been obtained for kasten and pilot cores from sites CON01-603 and CON01-605. This allowed... -
Infrared-Spectrometry on Cutting Samples of the KTB Main Hole (Drill Section ...
Infrared-Spectrometry on Cutting Samples of the KTB Main Hole (Drill Section HB1a), 5596-6760 m. -
SAFOD borehole trajectory data in absolute coordinates (UTM) and in coordinat...
SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major... -
Geochemistry and age model of sediment core BDP96-1 (BDP-2-A)
Within the framework of the Baikal Drilling Project (BDP), a 192 m long sediment core (BDP-96-1) was recovered from the Academician Ridge, a submerged topographic high between... -
Radial Vp on Core Samples of the KTB Main Hole HB1
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 -... -
Electrical Resistivity of Mini Cores (Plugs) of the KTB Main Hole HB1g
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... -
Thermal Conductivity of Cores of the KTB Main Hole HB1g (measured data)
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... -
Down-core variations of the reversal angle of the ChRM for VER98-1-1 and VER9...
Selected intervals of down-core variations of normalised relative paleointensity, ChRM inclination and declination, and the reversal angle. (A) Core CON 01-603-2: numbers in the... -
Magnetic Susceptibility of Cuttings of the KTB Pilot Hole HB1g (special samples)
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... -
Downcore variations of total sulphur for VER98-1-14
Higher abundance of greigite during glacial intervals coincides with small increases of the S content (Fig. 11B). Greigite levels in glacial sediments cannot be correlated... -
Wet bulk density (GRAPE) of piston core CON01-604-2 from Posolskoe, PANGAEA
Wet bulk density (GRAPE) of piston core CON01-604-2 from Posolskoe -
XRF of Cuttings of the KTB Main Hole HB1h.
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... -
Ultrasonic Seismics on Mini Cores (Plugs) of the KTB Main Hole HB1
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 -... -
SAFOD Main Hole downhole logging data phase 1.2, 2812-3043m
SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major... -
Electrical Resistivity of Cores of the KTB Main Hole HB1
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... -
SAFOD Main Hole downhole logging data phase 1.2, 2583-2812m
SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major... -
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...
