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SAFOD Main Hole downhole logging data phase 2 (2005), 3387-3799m
SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major... -
Natural Gamma-ray Activity of Cuttings of the KTB Main Hole HB1g (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... -
Axial Vs 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 -... -
Data for the relative percentages of the dominant diatom taxa related to core...
Dissolution was high throughout the profile—in most cases, only 10–20% of the valves considered as pristine (Fig. 4). High relative percentages of A. baicalensis and of benthic... -
Vertical profiles of settling particles in the water column.
During 16 months of deployment, 239 g m−2 dry matter settled in the 40-m trap, with an average flux of 14.9 g m−2 month−1 (Table 2 and Fig. 2). The content of organic carbon was... -
SAFOD Main Hole downhole logging data phase 1.2 1556-1744m
SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major... -
Water content and dry bulk density of pilot core CON01-604-2a to piston core ...
Water content and dry bulk density of pilot core CON01-604-2a to piston core CON01-604-2 from Posolskoe -
Axial Vs on Core Samples of the KTB Pilot Hole VB1
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 -... -
Axial Vs on Core Samples of the KTB Main Hole HB1a
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 -... -
Thermal Conductivity of Cuttings of the KTB Main Hole HB1a (measured 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... -
Water content and dry bulk density of pilot core to CON01-603-2, PANGAEA
Water content and dry bulk density of pilot core to CON01-603-2 -
Thermal Conductivity of Cuttings of the KTB Main Hole HB1i (measured 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... -
Density of Core Samples of the KTB Main Hole HB1g
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... -
Thermal Conductivity of Cuttings of the KTB Main Hole HB1g (measured 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... -
Permeability of Mini Cores of the KTB Main Hole HB1
In the KTB field laboratory, porosity, internal surface and permeability were determined on identical mini cores with 25.4 mm in diameter and approximately 50 mm in length.... -
Natural Gamma-ray Activity of Cuttings of the KTB Main Hole HB1 (measurements...
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... -
Thermal Conductivity of Cuttings of the KTB Main Hole HB1 (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... -
Density of Cuttings of the KTB Pilot Hole Vb1
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... -
Thermal Conductivity of Cores of the KTB Pilot Hole VB1a (transformed 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... -
Raw pollen data from the Eemian core CON01-603-2
The studied core CON01-603-2 was recovered from the Continent site, Northern Basin from a water depth of 386 m (Fig. 1) (see Charlet et al., 2005-this volume). The analysed...