main crystallization, the dike-like, true (or dilatation) aplite and small pegmatite nests were formed as the products of magmatic differentiation. Finally, in the third (so-called dike-forming) stage, the granite was cross-cut by dike swarms of
Authors:S. Ahmed, U. Faridi, M. Shahid, and M. Nisar
Abdullahi, J., Uvah, I.I., Dike, M.C. 1999. Life cycle and host preference studies of the Lesser grain borer Rhizopertha dominica F. on some common host food materials in Samaru, Nigeria. In: Dike, M.C., Ajayi, O., Okunade
Authors:Hajar Kazemi, Kouros Yazdjerdi, Abdolmajid Asadi, and Mohammad Reza Mozafari
. (2008) , Yamaji et al. (2010) , Yamaji and Sato (2011) , Bigi et al. (2013) , Andre and Milen (2014) , Yamaji (2016b) , and Shahamiri et al. (2017) , have specifically and systematically studied structures such as joints, dikes and mineral veins
Deutsch, A. 1984: Young Alpine dykes south of the Tauern Window (Austria): a K-Ar and Sr isotope study. -- Contrib. Mineral. Petrol., 85, pp. 45-57.
Young Alpine dykes south of the Tauern Window (Austria): a K-Ar and Sr isotope