Numerical heat and fluid flow modeling of the Hercynian Draa Sfar polymetallic (Zn–Pb–Cu) massive sulfide deposit, Central Jbilets, Morocco

A Review of Geotechnical Instabilities Identification and Monitoring At Deep Underground Mines: Case of Draa Sfar Mine in Morocco

“…The following units are distinguished [19], and  Joint sets Draa Sfar formations underwent a series of deformations, summarised in three stages of different intensity. We distinguish the DI compressive stage, represented by S1 schistosity and folding, the DII stage, represented by S2 schistosity, and the DIII brittle stage, represented by NNW faults [17].…”