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Hysteresis measurements (uncorrected and corrected for the paramagnetic influ...
Hysteresis measurements of a hematite dominated diatomaceous layer with pseudosingle to multidomain behaviour of the hysteresis loop for VER98-1-1. -
Magnetic field uplog, 19990705 for HSDP-2-A (592.5 m - 998.5 m)
A quasi-continuous magnetic log has been obtained in the Hawaii Scientific Drilling Project 2 (HSDP-2) between 600 m and 1800 m, which corresponds to a time interval of... -
Borehole Temperature of HSDP-2-A on 07/02/1999
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 chlorophyll a/carbon ratio (Chla/C), chlorophyllide a/carbo...
Fig. 4 visualises differences in the degradation between the organic compounds, chlorophylls, and carbon. The chlorophyll a/carbon ratio decreased with depth, indicating that... -
Diatom-inferred snow accumulation models for BAIK38 (BAIK94-38A) using uncorr...
Diatom-inferred snow depth reconstructions for BAIK38 using uncorrected taxa (Fig. 5a–c) show similar trends throughout the study period, with all or only five taxa in the... -
Wet bulk density (GRAPE) of piston core CON01-603-2 from CONTINENT Ridge
Wet bulk density (GRAPE) of piston core CON01-603-2 from CONTINENT Ridge -
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... -
Geochemical Analysis of Anions of Mud Samples of the KTB Pilot Hole VB1b.
Geochemical Analysis of Anions of Mud Samples of the KTB Pilot Hole VB1b. -
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... -
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... -
Borehole Temperature of HSDP-2-A on 13./14. April 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... -
Vector endpoint data for CON01-603-2.
Three representative vector endpoint diagrams: (A) sample from a clay-rich layer, exhibiting normal polarity; (B) sample from a clay-rich layer, exhibiting reverse polarity,... -
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... -
Magnetic Susceptibility of Cuttings of the KTB Pilot Hole VB1b
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... -
Down-core variations of the SIRM for CON01-603-2.
The concentration in ferromagnetic particles is much lower in the interglacial sediments than in glacial sediments. Therefore, the NRM needs to be normalised by a... -
Paleomagnetic measurements on sediment core BDP-1-A (BDP93-1).
We made magnetic measurement of 32 cubic specimens of sub-bottom sediments of Lake Baikal. These are part of the sub-samples for palaeomagnetic investigations obtained from the... -
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 -... -
Natural Remanent Magnetisation of Cores of the KTB Pilot Hole VB1
Natural Remanent Magnetisation of Cores of the KTB Pilot Hole VB1