Replication Data for: The magmatic-hydrothermal transition in pegmatites and its effects on rare-metal mineralization: Insights from melt-crystal-fluid interactions in phosphate minerals from the Buranga dike (Rwanda) - PhD Thesis

The enclosed datasets were acquired as part of the research of Fernando Prado Araujo towards obtaining the degree of Doctor of Science (PhD): Geology at the KU Leuven, Belgium. The purpose of the analyses is to understand the processes occurring during the transition from a melt- to a fluid-dominated environment in phosphorus-rich rare-element pegmatites. All measurements were performed in natural rock and mineral samples from the Buranga pegmatite, western Rwanda. Specifications of each dataset and measurement method are provided in the following sections.

Publication year:2022

Accessibility:open

Publisher:KU Leuven RDR

License:CC-BY-NC-SA-4.0

Format:txt, csv, jpg, tif, pdf, doc

Keywords: Fluid inclusions, Microscopy, Microthermometry, Mineral chemistry, Phosphate minerals, Raman spectroscopy, Trace element geochemistry, magmatic-hydrothermal, pegmatite