Structures of the fibrous dolomite crystals in methane seep carbonates from Marmorito, northwest Italy


Samples were made into 100 μm rock slices. Points of interest were aligned to the beam and measured with φ scans +/− 25° at χ = 0°, 30°, 60° and 90°, respectively. Stepsize of φ was 1° and exposure time was 10 seconds. Results were converted to powder diffraction diagrams by the CrysAlisPro software package.

Measurement name: Synchrotron X-ray diffractionInstrument: Beamline P24Place: Desy, HamburgEnergy: 24.79 keVBeam size: 50 x 50 µm²Sample detector distance: 400 mm

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Creator Lu, Yang ORCID logo; Paulmann, Carsten; Mihailova, Boriana ORCID logo; Malcherek, Thomas; Birgel, Daniel; López Correa, Matthias ORCID logo; Lin, Zhiyong ORCID logo; Lu, Liuyi; Milker, Yvonne ORCID logo; Peckmann, Jörn ORCID logo
Publisher PANGAEA
Publication Year 2023
Rights Creative Commons Attribution 4.0 International;
OpenAccess true
Resource Type Dataset
Format application/vnd.openxmlformats-officedocument.spreadsheetml.sheet
Size 56.9 kBytes
Discipline Earth System Research
Spatial Coverage (8.017 LON, 45.068 LAT)