87Sr/86Sr ratios in shallow and deep aquifers and thermal water from the eastern boundary fault of the northern upper Rhine Graben at the Heidelberg Basin, Germany: 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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| Hauptverfasser: | , , , , , , |
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| Dokumenttyp: | Article (Journal) Konferenzschrift |
| Sprache: | Englisch |
| Veröffentlicht: |
18 January 2017
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| In: |
Procedia earth and planetary science
Year: 2017, Jahrgang: 17, Pages: 108-111 |
| DOI: | 10.1016/j.proeps.2016.12.017 |
| Schlagworte: | |
| Online-Zugang: | Verlag, kostenfrei, Volltext: http://dx.doi.org/10.1016/j.proeps.2016.12.017
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| Verfasserangaben: | Gerhard Schmidt, Sami Al Najem, Margot Isenbeck-Schröter, Florian Freundt, Michael Kraml, René Eichstädter, Werner Aeschbach |
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| 245 | 1 | 0 | |a 87Sr/86Sr ratios in shallow and deep aquifers and thermal water from the eastern boundary fault of the northern upper Rhine Graben at the Heidelberg Basin, Germany |b 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 |
| 246 | 3 | 3 | |a 87 Sr / 86 Sr ratios in shallow and deep aquifers and thermal water from the eastern boundary fault of the northern upper Rhine Graben at the Heidelberg Basin, Germany |
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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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