Andere Kunden interessierten sich auch für
![Metamorphic Rocks of the Central Eastern Desert, Egypt]( "Metamorphic Rocks of the Central Eastern Desert, Egypt")
Metamorphic Rocks of the Central Eastern Desert, Egypt40,99 €![Integrated calcareous planktonic biostratigraphy, Eastern Desert Egypt]( "Integrated calcareous planktonic biostratigraphy, Eastern Desert Egypt")
Integrated calcareous planktonic biostratigraphy, Eastern Desert Egypt52,99 €![Gold deposits from Sink to Source in Southern Eastern Desert, Egypt.]( "Gold deposits from Sink to Source in Southern Eastern Desert, Egypt.")
Gold deposits from Sink to Source in Southern Eastern Desert, Egypt.64,99 €![Granitoides da mina de ouro Sukari, Deserto Oriental, Egipto]( "Granitoides da mina de ouro Sukari, Deserto Oriental, Egipto")
Granitoides da mina de ouro Sukari, Deserto Oriental, Egipto36,99 €![Geology and Archeological Heritage:]( "Geology and Archeological Heritage:")
Geology and Archeological Heritage:47,99 €![Depositional Evolution Of The Eocene Sediments, Fayum Area, Egypt]( "Depositional Evolution Of The Eocene Sediments, Fayum Area, Egypt")
Depositional Evolution Of The Eocene Sediments, Fayum Area, Egypt52,99 €![Hydrogeophysics and Structural Geophysics]( "Hydrogeophysics and Structural Geophysics")
Hydrogeophysics and Structural Geophysics36,99 €
The Sukari granitoid pluton is situated in the southern central Eastern Desert of Egypt and is considered as one of the best examples of the gold-bearing granites in the Arabian Nubian Shield (ANS).It consists of coarse- to medium-grained alkali-feldspar granite, syenogranite and monzogranite intruded the volcano-sedimentary sequences and metagabbro-diorite complex. Geochemically, these granitoids are metaluminous to peraluminous in character. Moreover, they show pronounced LREE-enriched patterns and negative Eu anomalies that indicate plagioclase fractionation. rocks are typical of within plate granites generated in tensional environment. They belong to ferroan/A-type granites, particularly A2-type suggesting post-collisional setting. Their high SiO2, Al2O3 and low MgO contents along with the low Ce/Pb ratios reflect derivation from melting crustal source. The kinematic indicators are represented by mylonites, quartz fish and augen structures. Mineralization in Sukari area foundas quartz veins, stockworks and brecciated veins.