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Swiss Journal of Geosciences
Fig. 6 | Swiss Journal of Geosciences

Fig. 6

From: Evidence of hydrothermal fluid flow in a hyperextended rifted margin: the case study of the Err nappe (SE Switzerland)

Fig. 6

Stable isotope data: δ18O versus δ13C cross plot for dolomite and calcite minerals from Piz Val Lunga (PVL) and Fuorcla Cotschna (FCT) areas; values are given relative to VPDB standard. The pink area corresponds to the first group of data described in the text (replacement dolomite and dolomite cements). The dashed lines encircle different mineral phases highlighting the difficulties to separate one group from another

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