Influence of mineralogical heterogeneities on the mechanical behavior of a shear zone in gneiss, Schauinsland Mine, Germany
Year: 2026
Type: article
Abstract: Enhanced geothermal systems including fault zones and fracture systems are characterized by geological heterogeneities leading to area dependent mechanical behavior. The interplay between fault zone porosity architecture and mechanical behavior is a key factor to understand the fault zone tectonic stability. Through the sampling across a clay-rich shear zone including host rock, transition zone and next to the main core zone, mechanical and mineralogical investigations presented a transition from a brittle to ductile failure behavior towards the main core zone. High compressive strength values were achieved for rock samples with high clay content which is an indicator of the reorganization of strong mineral phases within a weak compacted clayey matrix. Moreover, tensile strength parameters portrayed a decrease in strength towards the main core zone presenting a weakening effect due to the mineralogical composition. The increase in clay content related to the hydrothermal alteration of primary biotite and feldspar into clay minerals led to an increase in porosity. These different strength and hydraulic behaviors demonstrate the importance of the combined analysis of different disciplines to identify fault zone areas which are sustainable for geothermal exploitation.
Institutions: Technische Universität Darmstadt, GFZ Helmholtz Centre for Geosciences, Centre National de la Recherche Scientifique, Vrije Universiteit Brussel, Sorbonne Université, Institut des Sciences de la Terre de Paris, CY Cergy Paris Université, Bassins - Réservoirs - Ressources, Université de Picardie Jules Verne, Technische Universität Berlin
Language: English
Topic: Rock Mechanics and Modeling
Subfield: Mechanics of Materials
Field: Engineering
Domain: Physical Sciences
Open Access status: gold
Estimated APC paid: $3,890
Funder: European Commission
OpenAlex ID: W7141740782
