Eggeling, L., Schneider, S., Volland, S. (2017): Charakterisierung von Tiefengrundwasser zur nachhaltigen geothermischen Nutzung. bbr Leitungsbau Brunnenbau Geothermie. 3, 72-77.

Rolker, J., Schill, E., Stober, I., Schneider, J., Neumann, T., Kohl, T. (2015): Hydrochemical Characterization of a Major Central European Heat Flux Anomaly: The Bürchau Geothermal Spring System, Southern Black Forest, Germany. Geothermal Energy, 3 (1).

Schneider, J., Eggeling, L., Hesshaus, A. (2014): Analyse und Charakteristik von Tiefengrundwässern in Deutschland. In: Bauer, M., Freeden, W., Jacobi, H., Neu, T.: Handbuch Tiefe Geothermie (2014), Springer, 559-594.

Schroeder, H. and Schneider, J. (2014): Powerful Production Pumps to lift the Economy of Deep Geothermal Projects. In: Fuerst, W. and Bauernschmitt, J. (2014): Environment and Energy in Bavaria, München, 31-34. Download

Eggeling L. and Schneider J. (2012): Fluid monitoring during operation. In: Dittmann E. und Schneider J. (2012): Short Course 2012 – Aspects of Geothermal Power Plants in Operation, 8-12.

Schneider J., Bakker R.J., Bechstaedt T. & Littke R. (2008): Fluid evolution during burial diagenesis and subsequent orogenetic uplift: the La Vid Group (Cantabrian Zone, Northern Spain). Journal of Sedimentary Research, 78, 282-300

Schneider, J., Bechstädt, T. & Machel, H. (2004): Covariance of C- and O-isotopes with magnetic susceptibility as a result of burial diagenesis of sandstones and carbonates – an example from the Lower Devonian La Vid Group, Cantabrian Zone, NW Spain.- Int. J. Earth Sc., 93 (6), 990-1007.

Schneider, J., De Wall, H., Kontny, A., & Bechstädt, T. (2004): Magnetic susceptibility variations in carbonates of the La Vid Group (Cantabrian Zone, NW-Spain) related to burial diagenesis.- Sediment. Geol., 166, 73-88.



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