Ra’s Abdah of the north Eastern Desert of Egypt: the role of granitic dykes in the formation of radioactive mineralization, evidenced by zircon morphology and chemistry

Author:

Omran Ali A.,Dessouky Osama K.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology

Reference32 articles.

1. Bau M (1996) Controls on the fractionation of isovalent trace elements in magmatic and aqueous systems; evidence from Y/Ho, Zr/Hf, and lanthanide tetrad effect. Contrib Mineral Petrol 123:323–333

2. Bineli Betsi T, Lentz DR (2010) The nature of “quartz eyes” hosted by dykes associated with Au-Bi-As-Cu, Mo-Cu, and base-metal-Au-Ag mineral occurrences in the Mountain Freegold region (Dawson Range), Yukon, Canada. J Geosci 55:347–368

3. Breiter K (2002) From explosive breccia to unidirectional solidification textures: magmatic evolution of a phosphorus- and fluorine-rich granite system (Podlesí, Krušné hory Mts., Czech Republic). Bull Czech Geol Surv 77:67–92

4. Cemal Köksal S, Göncuoglu M, Toksoy-Köksal F, Möller A, Kemnitz H (2008) Zircon typologies and internal structures as petrogenetic indicators in contrasting granitoid types from central Anatolia, Turkey. Mineral Petrol 93:185–211

5. Corfu F, Hanchar JM, Hoskin PWO, Kinny P (2003) Atlas of zircon textures. In: Hanchar JM, Hoskin PWO (eds) Zircon. Reviews in mineralogy and geochemistry. Mineralogical Society of America, Chantilly

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