Replication Data for: Fluid exsolution during disequilibrium crystallization in the border and wall zones of internally zoned pegmatites

The datasets contain microthermometry, Raman spectroscopy and LA-ICP-MS results from fluid inclusions trapped in tourmaline and quartz for the paper: “Fluid exsolution during disequilibrium crystallization: Evidence from the border and wall zone of the Emmons Pegmatite (Maine, USA)”. The purpose of the analyses is to examine the fluid properties and compositions of the fluid inclusions and see if any changes occur within different crystal morphologies. All measurements were done on natural rock samples from the Emmons pegmatite in Maine, USA.