Complete Fission Track dating facilities are available at the FU Berlin. We have a fully equipped mineral separation laboratory for concentrating apatite and zircon. Facilities for mounting, polishing, and etching samples are in collaboration with University of Potsdam. We host a Zeiss © Axioplan 2 microscope with a maximum magnification of 1250 x paired with a Drawing Board VI ©, stage control, LED courser mouse and the FT Stage © software for counting and length measurements. Data record and …

The grain size composition can be determined with a laser diffractometer from Beckman-Coulter. The laser particle analyzer LS 13320 simultaneously measures the range from 2 mm to 40 nm. The laser particle analyzer uses the different light scattering of particles of different sizes.
We also perform particle size determinations for external customers. If you are interested and have any questions, please contact the laboratory manager

The laboratory for microscopy focuses on the specific requirements of microfacies analysis of lake sediments, but also offers a wide range of possibilities for other applications. Sedimentological, petrographic and microfacies analyses on all kinds of covered and uncovered thin sections and polished sections with transmitted and incident light are performed.

The laboratory for XRF (X-ray Fluorescence) Element Scanning focusses on non-destructive and continuous core analyses. These analyses allow detailed geochemical characterisation of complete sediment cores down to individual layers and grains. Bridging these scales is achieved by combining XRF core scanning, micro-XRF scanning of epoxy impregnated sediment blocks or thin sections, and Scanning Electron microscope (SEM) analyses.

The developments and research are focused on improving …

Petrography is a powerful tool to investigate rocks samples and loose preparates. By means of a microscope we characterize the morphology, texture and mineralogy of the components as well as to describe post-depositional features (diagenesis). This enables us to perform environmental, biostratigraphic and stable isotope analyses, as well as pore-system evolution studies. Additionally we use Digital Image Analysis to quantify sedimentary fabrics and pore space structures.

In our petrophysics lab, we aim to unravel the complicated relationship between porosity and permeability in sedimentary rocks, reconstruct the origin and modification of the analyzed pore system throughout its paragenetic evolution, and precisely detect small-scale heterogeneities of petrophysical properties. Such detailed and comprehensive pore system analysis does not only complement to the understanding of the depositional and diagenetic rock-forming processes, but is of absolute essence …

The preparation lab offers different preparation methods such as thin-section production, polishes, dye methods, hardening methods and others.

In the SedLab we analyze the compositional properties of sediments. Measuring the full range of grain size distributions from a few nanometers to centimeters and determine the shape of each single grain. Disentangling sediments allows scientists to infer the history of the sediments, interpret sedimentary archives and learn about the processes that have generated and transported the sediments.
The SedLab of the geomorphology section is fully equipped lab for measuring routinely large …

The sediment processing laboratory is a space for preparing marine and non-marine sedimentary samples for microscopy and other analyses, which require individual components or fabric specific analysis (e.g., Mass Spectrometry, trace metals, isotope studies…). Preparation methods include separating and picking of biogenic particles, thin section dying techniques, sieving for granulometry, and creating smear slides and acetate peels.

The sedimentology lab at the Permafrost Research section aims to study the transport and accumulation processes of permafrost-related deposits and classify sediment sequences in general. Therefore, the following parameters are investigated: sediment structure description, grain-size distribution and mass specific magnetic susceptibility.