Geological and structural studies on the Dara and Um Balad areas, North Eastern Desert, Egypt | ||
| Frontiers in Scientific Research and Technology | ||
| Volume 6, Issue 1, August 2023 PDF (1.45 M) | ||
| Document Type: Original Article | ||
| DOI: 10.21608/fsrt.2023.210738.1093 | ||
| Authors | ||
| Noha E. Baghdady* 1; Hassan I. El-Sundoly2 | ||
| 1Department of Geology, Faculty of Science, Damanhur University | ||
| 2Egyptian Mineral Resources Authority, Cairo, Egypt | ||
| Abstract | ||
| Metavolcanic, metagabbro-diorite, granodiorite, Dokhan volcanic, monzogranite, and alkali feldspar granite rocks covered Dara area. In contrast, metagabbro-diorite, Dokhan volcanic and monzogranite rocks covered Um Balad area. The North Eastern Desert is dominated by tectonic faults and related joint sets system; the dominant trends are NE - SW and NW - SE structural trends. The Dara area was affected by the extensional deformation phases trending NNW - SSE, NW - SE, NE - SW, and NNE - SSW. While the Um Balad area is affected by extensional deformation phases trending NW - SE, NNW - SSE, and NE - SW directions. On the other hand, the Dara area is affected by the compressional deformation phases trending NE - SW, WNW - ESE, and ENE - WSW directions. Um Balad area is affected by compressional deformation phases trending WNW - ESE, NE - SW, and NNW - SSE directions. Mineralized tension joints are widely distributed with different trends in the study areas. Generally, the monzogranite is highly deformed rather than the metagabbro-diorite rocks in the Dara area. While the metagabbro- diorite rocks are the highly deformed rock type in the Um Balad area. | ||
| Keywords | ||
| North Eastern Desert; Dara; Um Balad; geological setting; structural elements | ||
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