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Thermal Conductivity of Cores of the KTB Main Hole HB1a (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... -
Analysis boundaries and lighting trends (2012-2018) for selected Internationa...
This dataset is related to the question of whether communities inside of certified "International Dark Sky Places" have different levels of lighting change in comparison to... -
Geochemical Analysis of Anions of Mud Samples of the KTB Pilot Hole VB1
Geochemical Analysis of Anions of Mud Samples of the KTB Pilot Hole VB1. -
Optical DSLR camera- and UAV footage of the remote Mount Michael Volcano, Sau...
The eleven islands of the South Sandwich volcanic arc are amongst the least explored places on Earth. The mostly glacier covered volcanoes are home to the largest penguin... -
Permeability of Mini Cores of the KTB Main Hole HB1a
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.... -
GRACE Geopotential GAC Coefficients GFZ RL06
Spherical harmonic coefficients that represent the sum of the ATM (or GAA) and OCN (or GAB) coefficients during the specified timespan. These coefficients represent anomalous... -
GRACE-FO Geopotential GAC Coefficients GFZ RL06
Spherical harmonic coefficients that represent the sum of the ATM (or GAA) and OCN (or GAB) coefficients during the specified timespan. These coefficients represent anomalous... -
XRD of Cores of the KTB Pilot Hole VB1a
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... -
Vertical distribution in the sediment of the different animal groups found in...
The vertical distribution of organisms in the sediment indicates that animals can be present as deep as 15 cm although at very low abundance at such depths (Fig. 4, Fig. 5 and... -
GRACE Geopotential GAD Coefficients GFZ RL06
Spherical harmonic coefficients that are zero over the continents, and provide the anomalous simulated ocean bottom pressure that includes non-tidal air and water contributions... -
Porosity of Mini Cores (Plugs) of the KTB Main Hole HB1d
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... -
GRACE Geopotential GAB Coefficients GFZ RL06
Spherical harmonic coefficients that represent anomalous contributions of the non-tidal dynamic ocean to ocean bottom pressure during the specified timespan. The anomalous... -
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. -
Composite OSG Logging Data from the PTA-2 borehole, Big Island, Hawai'i
Compilation of downhole logging data from the borehole PTA2 inside Bradshaw Army Camp in the saddle region between Mauna Kea and Mauna Loa on the Big Island of Hawai'i... -
Thermal Conductivity of Cuttings of the KTB Main Hole HB1d (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... -
Attenuation coefficients and station corrections for harmonized local magnitu...
In Bindi et al. (2019) a harmonized local magnitude scale across Europe has been derived using data disseminated by network operators through the European Integrated Data... -
Gas chromatography of gas samples of the KTB main hole HB1i
The main objective of this drilling fluid analysis was the detection of inflows of formation fluids. Therefore different gases dissolved in the drilling mud were measured... -
Natural Gamma-ray Activity of Cores of the KTB Pilot Hole VB1
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... -
A global database of radiogenic Nd and Sr isotopes in marine and terrestrial ...
The database presented here contains radiogenic neodymium and strontium isotope ratios measured on both terrestrial and marine sediments. It was compiled to help assessing... -
Ultrasonic Seismics on Mini Cores (Plugs) 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 -...