During the late Cryogenian–Ediacaran (650–542Ma), the Arabian–Nubian Shield (ANS)
underwent final assembly and accretion to the Saharan Metacraton concurrent with the …

Each year, thousands of tourists visit Egypt's Wadi Feiran region, which is one of the most
popular tourist sites in the Sinai Peninsula. The region's topography is distinctive and …

Four isolated metamorphic complexes located within post-collisional granitoids occupying
up to 70% of the total area, were distinguished in Sinai (Egypt) and Elat area (southern …

Multi-isotope study including whole-rock Nd–Sr, single zircon Hf, and SIMS δ 18 O analyses
of zircons sheds light on magma sources in the northernmost Arabian–Nubian Shield (ANS) …

Abstract The Egyptian Nubian Shield (ENS) represents the northwestern part of the Arabian‐
Nubian Shield and the northern extension of the East African Orogen. The ENS is regarded …

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 …

Abstract The Feiran–Solaf metamorphic complex of Sinai, Egypt, is one of the highest grade
metamorphic complexes of a series of basement domes that crop out throughout the Arabian …

Morphotectonic lineaments observed on the Sinai Peninsula in Egypt were auto-detected
from Shuttle Radar Topography Mission 90-m digital elevation model (DEM) and gravity grid …

Abstract Ion-microprobe U–Th–Pb geochronological data are presented for fourteen
samples from the Feiran–Solaf metamorphic complex in the Sinai Peninsula, Egypt. These …

The Katherina ring complex (KRC) in the central part of south Sinai, Egypt, is a typical ring
complex of late Neoproterozoic age (605–580 Ma). It was developed during the final tectono …