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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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Bibliographische Detailangaben
Hauptverfasser: Schmidt, Gerhard (VerfasserIn) , Al Najem, Sami (VerfasserIn) , Isenbeck-Schröter, Margot (VerfasserIn) , Freundt, Florian (VerfasserIn) , Kraml, Michael (VerfasserIn) , Eichstädter, René (VerfasserIn) , Aeschbach, Werner (VerfasserIn)
Dokumenttyp: Article (Journal) Konferenzschrift
Sprache:Englisch
Veröffentlicht: 18 January 2017
In: Procedia earth and planetary science
Year: 2017, Jahrgang: 17, Pages: 108-111
DOI:10.1016/j.proeps.2016.12.017
Schlagworte:
Konferenzschrift
Online-Zugang:Verlag, kostenfrei, Volltext: http://dx.doi.org/10.1016/j.proeps.2016.12.017
Volltext
Verfasserangaben:Gerhard Schmidt, Sami Al Najem, Margot Isenbeck-Schröter, Florian Freundt, Michael Kraml, René Eichstädter, Werner Aeschbach
Beschreibung
Zusammenfassung: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.
Beschreibung:Im Zusatz zum Titel sind die Zahlen hochgestellt
Gesehen am 15.03.2017
Beschreibung:Online Resource
DOI:10.1016/j.proeps.2016.12.017

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