Cite
The South Um Mongul Cu-Mo-Au prospect in the Eastern Desert of Egypt: From a mid-Cryogenian continental arc to Ediacaran post-collisional appinite-high Ba-Sr monzogranite.
MLA
Abd El-Rahman, Yasser, et al. “The South Um Mongul Cu-Mo-Au Prospect in the Eastern Desert of Egypt: From a Mid-Cryogenian Continental Arc to Ediacaran Post-Collisional Appinite-High Ba-Sr Monzogranite.” Ore Geology Reviews, vol. 80, Jan. 2017, pp. 250–66. EBSCOhost, https://doi.org/10.1016/j.oregeorev.2016.06.004.
APA
Abd El-Rahman, Y., Seifert, T., Gutzmer, J., Said, A., Hofmann, M., Gärtner, A., & Linnemann, U. (2017). The South Um Mongul Cu-Mo-Au prospect in the Eastern Desert of Egypt: From a mid-Cryogenian continental arc to Ediacaran post-collisional appinite-high Ba-Sr monzogranite. Ore Geology Reviews, 80, 250–266. https://doi.org/10.1016/j.oregeorev.2016.06.004
Chicago
Abd El-Rahman, Yasser, Thomas Seifert, Jens Gutzmer, Amir Said, Mandy Hofmann, Andreas Gärtner, and Ulf Linnemann. 2017. “The South Um Mongul Cu-Mo-Au Prospect in the Eastern Desert of Egypt: From a Mid-Cryogenian Continental Arc to Ediacaran Post-Collisional Appinite-High Ba-Sr Monzogranite.” Ore Geology Reviews 80 (January): 250–66. doi:10.1016/j.oregeorev.2016.06.004.