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

Author:

Schmidt Gerhard,Najem Sami Al,Isenbeck-Schröter Margot,Freundt Florian,Kraml Michael,Eichstädter René,Aeschbach Werner

Publisher

Elsevier BV

Subject

General Engineering

Reference8 articles.

1. Freundt F, Al Najem S, Aeschbach-Hertig W, Isenbeck-Schröter M, Schmidt G, Grobe R, Kraml M. A multi-tracer approach for the exploration of deep geothermal energy potential and fault zone characterisation, applied in the Upper Rhine Graben. Geophysical Research Abstracts 2014;Vol. 16: EGU2014-13059.

2. Salinization of shallow groundwater by a deep fluid ascending at the western main fault zone of the northern Upper Rhine Graben;Al Najem;Germany: Discussion of the origin and evolution using major and trace element compositions. Submitted to Applied Geochemistry,2016

3. Source and origin of active and fossil thermal spring systems;Loges;northern UpperRhine Graben, Germany. Appl, Geochem,2012

4. Paleogene phreatomagmatic volcanism on the western main fault ofthe northern Upper Rhine Graben;Lutz;(Kisselwörth diatreme and Nierstein – Astheim Volcanic System Germany). Bull Volcanol,2013

5. Rare earth elements and Sr and Nd isotopic compositions of dissolved and suspended loads from small river systems in the Vosgesmountains (France), the River Rhine and groundwater;Tricca;Chemical Geology,1999

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