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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.

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Czech Geological Survey
Geologická 577/6
152 00 Praha 5
phone: +420251085322