Geological and petrological studies using remote sensing applications at Wadi Khuda-Wadi Shut area, South Eastern Desert, Egypt
Mahmoud Mostafa Abd el Hamid Shokry;
Abstract
Wadi Khuda-Wadi Shut area in the south Eastern Desert (SED) of Egypt is located on the Red Sea Coast about 180 km south Marsa Alam City, between latitudes 23° 33' and 23° 50' N and longitudes 35° 05' and 35° 26' E.
The area is built up of Pan-African Precambrian basement rocks of metamorphic and magmatic assemblages. The metamorphic one comprises gneisses-migmatites, ophiolitic serpentinites and island-arc metavolcanics. These rock units are intruded by syn - to late - tectonic magmatic assemblage of diorite, granodiorite, ultramafic-mafic association, and syenogranite intrusions. The whole sequence is traversed by post tectonic dykes, veins and quartz plug.
The area is built up of Pan-African Precambrian basement rocks of metamorphic and magmatic assemblages. The metamorphic one comprises gneisses-migmatites, ophiolitic serpentinites and island-arc metavolcanics. These rock units are intruded by syn - to late - tectonic magmatic assemblage of diorite, granodiorite, ultramafic-mafic association, and syenogranite intrusions. The whole sequence is traversed by post tectonic dykes, veins and quartz plug.
Other data
| Title | Geological and petrological studies using remote sensing applications at Wadi Khuda-Wadi Shut area, South Eastern Desert, Egypt | Other Titles | دراسة جيولوجية وبترولوجية باستخدام تطبيقات الاستشعار عن بعد لمنطقة وادى خوده - وادى شوت، جنوب الصحراء الشرقية ، مصر | Authors | Mahmoud Mostafa Abd el Hamid Shokry | Issue Date | 2020 |
Attached Files
| File | Size | Format | |
|---|---|---|---|
| BB1343.pdf | 193.89 kB | Adobe PDF | View/Open |
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