Description
Precipitated calcite coating is often observed within water-conducting features (calcite veins), affecting the hydraulic and geochemical properties of these features. Indeed, the presence of such a coating is evidence that the feature conducts (or has at some time conducted) flowing water. Only minor calcite precipitation was observed in the Opalinus Clay, giving strong palaeohydrogeological evidence for the long-lasting absence of flowing water.
OPA Category
Category as used in the OPA assessment
OPA host rock
OPA Number
Number as used in the OPA assessment
1.10
Screening
Screening basis for screened out FEPs
NA
NEA V1 IFEP Reference(s)
Related IFEPs from the NEA V1 IFEP list from 1999
2.2.02, 2.2.07, 2.2.05