Ascending deep fluids into shallow aquifer at hydraulically active segments of the western boundary fault of the Rhine Graben, Germany: constraints from 87Sr/86Sr ratios : 15th Water-Rock Interaction International Symposium, WRI-15
87Sr/86Sr ratios have been used as a tracer of fault-controlled fluid ascent into shallow aquifers at the Western Boundary Fault (WBF) of the northern upper Rhine Graben in Germany, a major rift system of the European continent. The 87Sr/86Sr ratios and Sr contents from the Quarternary groundwater c...
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| Main Authors: | , , , , , , |
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| Format: | Article (Journal) Conference Paper |
| Language: | English |
| Published: |
18 January 2017
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| In: |
Procedia earth and planetary science
Year: 2017, Volume: 17, Pages: 81-84 |
| DOI: | 10.1016/j.proeps.2016.12.001 |
| Subjects: | |
| Online Access: | Verlag, kostenfrei, Volltext: http://dx.doi.org/10.1016/j.proeps.2016.12.001 Verlag, Volltext: http://www.sciencedirect.com/science/article/pii/S1878522016300339 
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| Author Notes: | Gerhard Schmidt, Sami Al Najem, Margot Isenbeck-Schröter, Florian Freundt, Michael Kraml, René Eichstädter, Werner Aeschbach |
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| 245 | 1 | 0 | |a Ascending deep fluids into shallow aquifer at hydraulically active segments of the western boundary fault of the Rhine Graben, Germany |b constraints from 87Sr/86Sr ratios : 15th Water-Rock Interaction International Symposium, WRI-15 |c Gerhard Schmidt, Sami Al Najem, Margot Isenbeck-Schröter, Florian Freundt, Michael Kraml, René Eichstädter, Werner Aeschbach |
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| 520 | |a 87Sr/86Sr ratios have been used as a tracer of fault-controlled fluid ascent into shallow aquifers at the Western Boundary Fault (WBF) of the northern upper Rhine Graben in Germany, a major rift system of the European continent. The 87Sr/86Sr ratios and Sr contents from the Quarternary groundwater conducting sediments of the uppermost aquifer increase with decreasing distance to the WBF. The 87Sr/86Sr ratios and Sr contents of the shallow groundwater range from 0.70877 to 0.71022 and 0.41 to 2.30 mg/l, respectively. The Strontium isotope ratios are important tracers of hydrological processes such as water-rock interaction and groundwater mixing at active faults and thus a powerful geochemical tool for the detection of the ascent of deep fluids at hydraulically active segments of faults and its mixing with shallow recharged groundwater. | ||
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