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K2O diagram. HK: high-K; MK: medium-K; CA: calc-alkaline; Alk Bas: alkali basalt; HK CA: high-K calc-alkaline volcanics; MK CA: medium-K calc-alkaline. Eliwa et al. (2006) noted that the Dokhan Volcanics from Wadi Um Sidra and Um Asmer range from medium- to high-K alkali basalt to rhyolite. They comprise voluminous medium- to high-K calc-alkaline lavas, subordinate adakitic lavas, and minor alkali basalt. 4. Adakitic lavas contain very low Y (<18 ppm) and heavy REE (HREE; Yb≤1 ppm) 40 contents, with high Sr (>750 ppm) and Sr/Y (>40).

In: S. O. Greiling (Editors), The Pan-African belt of Northeast Africa and Adjacent Areas. Friedr Viewgsohn, Braunschweig/Wiesbaden, pp. 175-184. , 1972. A new geological map for the basement rocks in the eastern and southwestern deserts of Egypt. Egypt Geol. Survey Annals, 2: 1-18. , 2006. Geochemistry and petrogenesis of the post-orogenic bimodal dyke swarms in NW Sinai, Egypt: Constraints on the magmatic-tectonic processes during the late Precambrian. Chemie der Erde, 66: 129-141. , Furnes, H.

In later centuries, porphyry columns and other pieces were widely reused in new constructions, often reappearing far from their original Roman context. In 786, Charlemagne received permission from Pope Hadrian to remove classical columns of porphyry from Rome to build his cathedral at Aachen. The renaissance Medici family commissioned portrait busts carved from porphyry blocks that had been warehoused in 53 Rome since imperial times. Other sources are unknown and unguessable: The Victoria and Albert Museum in London contains a pair of fine porphyry earrings.

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