Trace elements, δ13C, δ18O and 87Sr/86Sr of cave-filling giant crystalline calcites and fluid inclusion homogenization temperatures (HTs) were analyzed from each formation in the Eopalaeozoic carbonate reservoirs. The result shows that the giant crystalline calcite samples in different wells may have various fluid origins. The characters of 87Sr/86Sr-rich and low δ18O values suggest that this low temperature fluid should be derived from meteoric water.