Abstract:
Hydrothermal paleokarst cavities with calcite crystals up to 20 cm in diameter were found in two caves of the Nizke Tarry Mountains developed in Triassic limestone and dolomite of the Guttenstein type. In both caves, older zones of tectonic and hydrothermal activity have been overprinted by vadose speleogenesis. According to fluid inclusion microthermometry data, prismatic-scalenoliedral calcite from the Silvo ova Diera Cave has precipitated at temperatures between similar to60 and 101degreesC from low salinity aqueous solutions (less than or equal to0.7 wt. % NaCl eq.). Carbon and oxygen isotope profiling revealed significant delta(13)C decrease accompanied by slight delta(18)O increase during growth of calcite crystals. The negatively correlated carbon and oxygen isotope data cannot be interpreted in terms of any geologically reasonable models based on equilibrium isotopic fractionation. Fluid inclusion water exhibits minor decrease of deltaD values from crystal core (-31 %o SMOW) to rim (-41 %(0) SMOW). Scalenohedral calcite from the NovA Stanisovska Cave has precipitated at slightly higher temperatures 63-107degreesC from aqueous solutions with salinity : less than or equal to2.7 % NaCl eq. The positively correlated trend of delta(13)C and delta(18)O values is similar to common hydrothermal carbonates. The fluid inclusion water deltaD values differ significantly between the crystal core (-50 %(0) SMOW) and rim (- 11 %o SMOW). The calcite crystals are interpreted as representing a product of an extinct hydrothermal system, which was gradually replaced by shallow circulation of meteoric water. Fossil hydrothermal fluids discharged along Alpine uplift-related NNW-SSE-trending faults in Paleogene-pre-Pliocene times. Increased deuterium concentration in the inclusion water compared to recent meteoric precipitation indicates a warmer climate during the calcite crystallization