Creation of Secondary Porosity in Dolostones by Upwelling Basement Water in the Foreland of the Alpine Orogen

Figure 14

Wetherill concordia diagrams illustrating the results of the LA-ICP-MS analyses of secondary calcites in the Muschelkalk (MK) and the crystalline basement (CB) at the wells of Benken (BEN), Schlattingen (SLA), Siblingen (SIB), and Leuggern (LEU). The error ellipses correspond to two standard deviations of the mean.

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