Timing of the Granite magmatism, Wadi Abu Abid, North Eastern Desert, Egypt | ||
| Alfarama Journal of Basic & Applied Sciences | ||
| Volume 6, Issue 4, October 2025, Pages 464-479 PDF (1.35 M) | ||
| Document Type: Original Article | ||
| DOI: 10.21608/ajbas.2025.405510.1270 | ||
| Authors | ||
| Mohamed Ali Gharib* ; Mohammed Zaky El-Bialy; Mohamed Mohamed Omar; Sherif Mansour | ||
| Geology Department, Faculty of Science, Port Said University, Port Said 42522, Egypt | ||
| Abstract | ||
| Granitic rocks represent a large portion of the Arabian-Nubian Shield (ANS) exposures in the North Eastern Desert (NED). The timing of the magmatic events plays a major role in illustrating the ANS development. In order to evaluate the ANS, it is important to understand their geochronological order. Therefore, we studied calc-alkaline and alkaline granitic samples from Wadi Abu Abid, Gabal Um Anab area, North Eastern Desert, Egypt, to chronologically evaluate the ANS magmatic process in the studied region. The results show ages of the syn-collisional compressional magmatic event for all the analyzed samples. The resulting ages extended from 755 ± 16 Ma to 667 ± 15 Ma, which represents some conflicts with the traditional classification of the granitoids as being either Older syn-collisional calc-alkaline granitoids or Younger post-collisional alkaline granitic rocks. Xenocrysts with pre-ANS ages noted in five zircon grains in two samples, given ages of 2006 ± 85 Ma, 1887 ± 84 Ma, 1616 ± 73 Ma, 1228 ± 73 Ma, and 1227 ± 70 Ma, which suggest a local rework of an older magmatic source. | ||
| Keywords | ||
| Older granites; North Eastern Desert; magmatic events; Zircon U-Pb dating; Arabian–Nubian Shield | ||
|
Statistics Article View: 177 PDF Download: 62 |
||
