“…The study area field checking was dominated by a high intensity of hydrothermal alteration, which affected many rocks that embedded mineral types such as chlorite, epidote, muscovite, or sericite, and opaque minerals. The altered mineralized rocks display secondary minerals, which are common indicators of mineralization, such as gold and copper (Gabr, Ghulam, & Kusky, 2010; Han & Nelson, 2014; Liu, Li, Zhou, Han, & Xu, 2018; Ruiz‐Armenta & Prol‐Ledesma, 1998). Zoheir and Emam (2012) found that the alteration area, comprising pyrite, quartz, carbonate, chlorite, sericite, and goethite, hosts several open pits and trenches within quartz veins and boudins in Egypt.…”