Fig. 2 | Scientific Reports

Fig. 2

From: Fertile high-K magmatism and hydrothermal alteration zone associated with porphyry copper mineralization in Samra area, SE Sinai, Egypt

Fig. 2

(a) Metasediments in southwestern part of Samra area, (b) Metavolcanics alteration between lava sheet and pyrolcatics, (c) Massive dacite lava sheet, Wadi Kid area, (d) Altered dacite overlined by conglomerate, (e) NE-trending Kid Conglomerates belt (f) Post tectonic granites with rugged topography. intruding the volcano-sediments rocks.

Back to article page