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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 -
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... -
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... -
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... -
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... -
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... -
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... -
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... -
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... -
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... -
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... -
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... -
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... -
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... -
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... -
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...
