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Fig. 9 | Swiss Journal of Geosciences

Fig. 9

From: Sediment provenance during Alpine orogeny: fluid inclusions and stable isotopes on quartz–calcite veins from detritic pebbles

Fig. 9

Diagram showing the hydrogen and oxygen isotopic compositions of sedimentary rocks and magmatic/metamorphic rocks in the range of studied samples (modified from Hoefs 2009) (See Table 2 for δD and δ18O data). The Global Mean Water Line is also represented, summarizing the composition of meteoric waters. The obtained δD and δ18O values from the studied samples are plotted and indicate a deep origin of the fluid trapped in the veins during their crystallization

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