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Gas Mass Spectrometry of Gas Samples of the KTB Pilot Hole VB1b
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... -
Gas Mass Spectrometry of Gas Samples of the KTB Main Hole HB1
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... -
Downcore variations of SIRM/κLF for CON01-603-2
Increased presence of greigite (high SIRM/κLF) coincides with maximum sulphur contents observed at the beginning of interglacial stages (Fig. 11A). At similar levels in another... -
Downcore variations of the TOC and TS for VER 98-1-14
Total organic carbon (TOC) and total sulphur (TS) were determined using a LECO CS-225-Analyser. The clay-rich layers are characterised by low levels of TOC and TS. The... -
XRF of Centrifuge Samples of the KTB Pilot Hole VB1b.
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... -
XRD of Cuttings of the KTB Main Hole HB1i
The qualitative and quantitative phase analyses were performed in the KTB field laboratory by x-ray powder diffraction using SIEMENS D 500 diffractometer. During early stages of... -
Downcore variations of normalised relative paleointensity for CON01-603-2, VE...
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... -
Hysteresis measurements (uncorrected and corrected for the paramagnetic influ...
Hysteresis measurements of a magnetite dominated clay-rich layer with pseudosingle-domain behaviour of the hysteresis loop for VER98-1-1. -
Downcore variations of rock magnetic parameters for the sedimentary sequence ...
Downcore variations of rock magnetic parameters and simplified lithological description for the sedimentary sequence VER 98-1-14. Here, MIS are denoted by numbers in the... -
CONTINENT sampling positions and related projects
Sampling positions of the EU-project CONTINENT and related projects. The co-ordinates of the sampling positions were transformed from geograpical coordinates to UTM Z48, WGS 84.... -
Gamma Log for HSDP-2-A on 4. July 1999
The target of this study is to correlate the logging data with the lithological and structural characteristics of the drilled volcanic sequences; in particular to extract... -
Down-core variations of anhysteretic remanent magnetisation and simplified li...
Conceptual intercorrelation between ARM and simplified lithology and correlation to the δ18O record from ODP Site 677 (Shackleton et al., 1990), assuming that clay-rich layers... -
XRD of Cores of the KTB Main Hole HB1i
The qualitative and quantitative phase analyses were performed in the KTB field laboratory by x-ray powder diffraction using SIEMENS D 500 diffractometer. During early stages of... -
SAFOD Main Hole downhole logging data phase 1.2, 2353-2582m
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 Cores of the KTB Main Hole HB1a
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... -
Down-core variations of normalised relative paleointensity after removal of i...
Down-core variations of normalised relative paleointensity after removal of intervals affected by diagenesis (magnetite dissolution and/or greigite formation) and correlation to... -
Axial 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 -... -
XRD of Cuttings of the KTB Pilot Hole HB1
The qualitative and quantitative phase analyses were performed in the KTB field laboratory by x-ray powder diffraction using SIEMENS D 500 diffractometer. During early stages of... -
Porosity of Mini Cores (Plugs) of the KTB Pilot Hole VB1a
The porosity was determined using the most common Archimedian method (Schopper, 1982). It is based on the following three weight determinations of the sample: (1) The samples... -
Geochemical Analysis of Cations of Mud Samples of the KTB Pilot Hole VB1.
Geochemical Analysis of Cations of Mud Samples of the KTB Pilot Hole VB1.