Skip to main content
padlock icon - secure page this page is secure

Deep geothermal resources of the North German Basin: The hydrothermal reservoirs of the Stuttgart Formation (Schilfsandstein, Upper Triassic)

Buy Article:

$39.00 + tax (Refund Policy)

The enormous geothermal resources of the North German Basin are bound to Palaeozoic petrothermal and Mesozoic hydrothermal reservoirs. Based on previous exploration campaigns, six Mesozoic reservoir complexes were identified among which the hydrothermal reservoirs of the Stuttgart Formation were underexplored so far. To evaluate the potential of these reservoirs, an interdisciplinary exploration strategy was applied to a large database of cores, wireline logs and seismic data. Repeated transgressions from Tethyan waters resulted in formation of inland seas covering large parts of the basin. Accordingly, the deposition of the Stuttgart Formation was primarily controlled by 3 rd - and 4 th -order T-R sequences; in particular the basinwards-directed progradation of the fluvio-deltaic Lower and Upper Schilfsandstein members are related to lowstands. Within both members, fine- to medium-grained sandstones of channel fills and levee/crevasse splay complexes form compound reservoirs representing the main target of geothermal exploration. For the Lower Schilfsandstein, this channel belt reservoir type is characterised by a median thickness of 23 m, median porosity of 22.7 % and median permeability of 443 mD. For the Upper Schilfsandstein, the channel belt reservoir type is characterised by a median thickness of 17 m, median porosity of 24 % and median permeability of 546 mD. The quality of these reservoirs is limited by the generally low compositional maturity of sandstones being lithic arkoses and feldspatic litharenites, the partly high content of detrital matrix within pores and substantial diagenetic cementation. The resulting high lateral variability of reservoir qualities contributes to considerable exploration risks. Despite this, reservoirs of high quality could be proven for individual localities where they may be considered an alternative option if the development of Upper Keuper or Middle Jurassic hydrothermal reservoirs fails.
No Reference information available - sign in for access.
No Citation information available - sign in for access.
No Supplementary Data.
No Article Media
No Metrics


Document Type: Research Article

Publication date: September 1, 2018

More about this publication?
  • Zeitschrift der Deutschen Gesellschaft für Geowissenschaften (ZDGG) is an international peer reviewed journal that accepts papers on research and applied topics in the Earth Sciences. It is published online and in print. One volume, consisting of four issues is published annually. The journal has been published by the German Geological Society since its foundation in 1848. It was relaunched in 2005.

    ZDGG invites the submission of English, German and French language papers from all fields of geology, hydrogeology, paleontology, tectonics, sedimentology, engineering geology and of course environmental geology to name a few. The editors of ZDGG also invite suggestions for thematic issues.

    Please note that ZDGG issues from Volume 170 are now available from the publisher's website at
  • Editorial Board
  • Information for Authors
  • Subscribe to this Title
  • Access to Vol 170 onwards
  • Ingenta Connect is not responsible for the content or availability of external websites
  • Access Key
  • Free content
  • Partial Free content
  • New content
  • Open access content
  • Partial Open access content
  • Subscribed content
  • Partial Subscribed content
  • Free trial content
Cookie Policy
Cookie Policy
Ingenta Connect website makes use of cookies so as to keep track of data that you have filled in. I am Happy with this Find out more