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