Fluid inclusions

By microthermometric measuring of fluid inclusion is possible to study P-V-T-X properties of paleofluids in minerals and rocks form from different geological environment. Determination of composition, temperature and pressure of capture of paleofluids contributes to a complex stadium study, e.g. of a genesis of raw material deposits, diagenetic conditions in sedimentary environment and determination of a degree of metamorphosis and to the study of a fluid flow in different rocks as well.