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CTD profiles at hadal trench locations collected on the DSSV Pressure Drop be...
Conductivity-Temperature-Depth (CTD) observations were made from the DSSV Pressure Drop using full-depth hadal landers at sixteen of the world's trenches between 2018 and 2022.... -
Rheometric Analysis of Viscous Material Mixtures Used in the Tectonic Laborat...
This dataset contains measurements of viscous and viscoelastic materials that are used for analogue modelling. Proper density and viscosity scaling of ductile layers in the... -
Copepods from a sublittoral sandy station in the North Sea
Data on densities and species composition of copepods on a sublittoral sandy station (station 50) in the North Sea. -
MVP Data 2nd QC- EUREC4A_OA/ATOMIC
The EUREC4A-OA oceanographic campaign that took place in January-February 2020 in the tropical North-West Atlantic Ocean aboard several research vessels, was a contribution to... -
Phonon Density of States in Nanocrystalline YAG:Cr
Here we propose to measure the phonon density of states in nanocrystalline samples of YAG:Cr. Our parallel luminscence measurements have revealed dramatic changes in the phonon... -
Water proton's environment in Low Density and Very High Density Amorphous Ices
Amorphous polymorphism is one of the key concepts in our understanding of water, its structure, physical properties and anomalies. The basic idea is that liquid water at ambient... -
uCTD Data 2nd QC- EUREC4A_OA/ATOMIC
The EUREC4A-OA oceanographic campaign that took place in January-February 2020 in the tropical North-West Atlantic Ocean aboard several research vessels, was a contribution to... -
WOCE Global Ocean Climatology 1990-1998
Abstract: The World Ocean Circulation Experiment (WOCE) Global Hydrographic Climatology (WGHC) provides the basis for all maps of the WOCE Atlantic Atlas. This climatology... -
Porosity of Mini Cores (Plugs) of the KTB Main Hole HB1a
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... -
Density of Core Samples of the KTB Main Hole HB1i
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... -
Density of Cuttings of the KTB Main Hole HB1g
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... -
Porosity of Mini Cores (Plugs) of the KTB Main Hole HB1
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... -
Density of Cuttings of the KTB Main Hole HB1a
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... -
Density of Core Samples of the KTB Main Hole HB1a
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... -
Density of Core Samples of the KTB Main Hole HB1
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... -
Density of Core Samples 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... -
Density of Cuttings of the KTB Main Hole HB1d
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... -
Porosity of Mini Cores (Plugs) of the KTB Pilot Hole VB1
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... -
Natural Gamma-ray Activity of Cores 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... -
Density of Cuttings of the KTB Main Hole HB1i
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...
