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Chemical and U–Sr isotopic variations in stream and source waters of the Strengbach watershed (Vosges mountains, France)

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Figure

Figure 1. Map of the Strengbach catchment showing the principallithological units and the location of the 10 studied springs (SG,RH, ARG, BH, CS1, CS2, CS3, CS4, SH, RUZS)
Figure 2. Physico-chemical characteristics of the different source waters of the Strengbach watershed (average values for the period 2004–2006)
Figure 4. Relationships between0,09 0,06 0,03  87Sr/86Sr isotope ratios and (a) 1/Sr (ppb); (b) Ca/Sr (ppb ppb−1)
Figure 5. Relationship between (234U/238U) AR and (a) 1/U and, (b) 87Sr/86Sr. In contrast to Sr isotopic compositions, the U AR ofsprings do not allow to distinguish between the northern and southern slopes.
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