2021
DOI: 10.1127/zdgg/2021/0286
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Quantifying model uncertainty of a geothermal 3D model of the Cenozoic deposits in the northern Upper Rhine Graben, Germany

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Cited by 5 publications
(2 citation statements)
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“…Before discussing the results in this section, it is necessary to pin point some limitations of the calculated HIP. As for any model, there are uncertainties and a limited resolution in the basic geological model (Arndt et al 2011;Van Der Vaart et al 2021) as well as in the thermal models [discussed in Koltzer et al (2019a)]. Also the limitations related to the choice of parameters (physical properties and boundary conditions) set to derive the HIP need to be mentioned.…”
Section: Discussionmentioning
confidence: 99%
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“…Before discussing the results in this section, it is necessary to pin point some limitations of the calculated HIP. As for any model, there are uncertainties and a limited resolution in the basic geological model (Arndt et al 2011;Van Der Vaart et al 2021) as well as in the thermal models [discussed in Koltzer et al (2019a)]. Also the limitations related to the choice of parameters (physical properties and boundary conditions) set to derive the HIP need to be mentioned.…”
Section: Discussionmentioning
confidence: 99%
“…1b). Of these, the northwestern Rhenohercynian block crops out in the Rhenish Massif (Klügel 1997) and is followed southward by the Northern Phyllite Zone and the Mid German Crystalline High, cropping out in the Odenwald (Stein 2001;Franke 2000;Frey et al 2021;Weinert et al 2021).…”
Section: D Structural Model Of Hessementioning
confidence: 99%