Chronology of Neoproterozoic volcanosedimentary successions remains controversial for
many regions of the Arabian–Nubian Shield, including the Dokhan Volcanics of NE Egypt …

Origin and tectonic setting of the late Neoproterozoic Dokhan Volcanics (ca. 610–560Ma by
whole rock Rb–Sr and ca. 600–590Ma by SHRIMP U–Pb zircon) in the Egyptian Eastern …

The Neoproterozoic tectonic evolution of the Egyptian Eastern Desert (EED) basement is
documented, principally through its history of structural events, and to a lesser degree …

Located 100km northwest of Hurghada, the volcanosedimentary successions of Gebel El Urf
is exposed between latitude 27° 45′ 30 ″and 27° 51′ 00 ″N and longitude 32° 49′ 00 …

Dyke swarms traverse Neoproterozoic rocks in the Hawashiya region in the extreme
northern part of the Eastern Desert of Egypt. They are a suite of basaltic andesite and …

The present work deals with geology, geochemistry, radioactivity and tectonic environment
of the granitic and volcanic rocks at Hadarba area, South Eastern Desert of Egypt. The …

The area around Gabal (G.) Kherm El Asmar is occupied by metavolcanics, Dokhan
volcanics as well as different types of younger granite pertaining to the Syenogranites and …

The present work provides the geology, geochemistry, and petrogenesis of the Dokhan
volcanics rocksexposed at the areas surrounding Wadi Um Sidra and Wadi Um Asmer in the …

В данной статье мы представляем обзор самой молодой составляющей
фундаментального комплекса Восточной пустыни Египта-Формация Доханиских …

The present work deals with geology, geochemistry, radioactivity and tectonic environment
of the granitic and volcanic rocks at Hadarba area, South Eastern Desert of Egypt. The …