Abstract A detailed and fully coupled thermo-hydro-mechanical (THM) model for fractured rock is presented. This model distinguishes itself by harmoniously integrating elastoplastic material behaviour with a continuum damage mechanics framework. Solid matrix displacement. pore and fissure water pressures and temperature of the solid are introduced as the primary nodal variables. https://www.roneverhart.com/Tiamat-s-Rebuke-East-Non-Ladder/
Tiamats rebuke
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