Table 1 Rock units, lithology, and the corresponding ages in the WA area.

From: Radiometric characteristics of some metallic ores and nonmetallic deposits: an example, Wadi Al-Allaqi, South Eastern Desert, Egypt

Age

Rock units

Lithology

Late proterozoic

Meta-sedimentary rocks group

sericite biotite gneissic rocks (msp), sericite-rich schist (mss), talc, ankerite, and marble (mm)

Calc alkaline Volcanics and sub-volcanics group,

Intermediate to base volcanic rocks (VI-B), intermediate sub-volcanic chlorite-rich rocks (VI), intermediate sub-volcanic schist and tuffs rich in chlorite (MVIC), intermediate lava, tuffs, and agglomerate rocks (MVT), intermediate volcanic rocks rich in sericite (MVIS), undifferentiated intermediate volcanic sub-volcanic schist, and tuffs (MVI)

Ophiolite nappe /mélange group

Serpentine and talc (osta) at Jabal Shillman, Talc and ankerite (ota) at Wadi Haymur Ankerite, Quartz carbonate, and magnesian schist (oaq)

The young calc-alkaline volcanic sub-volcanic group includes

Rhyolite flows, tuffs and microgranite (mvr)

Syn to late tectonic granitoid (Older granites)

Quartz diorite (mgb), (mdq), and tonalite (mgt)

Post-tectonic mafic ultra-mafic intrusions

Gabbro (gbp), and Gabbro dolerite (gbh)

Post-tectonic potassic calc-alkaline granitoid (Younger granites)

Tonalite (gt), at Umm Ashira, Wadi Murrah, Wadi Shilman Mozogranite (gm), at Jabal Arakah,Rod Abu Nsir, Jabal Filat and Microgranite at Jabal Abu Sayal (qf)

Paleozoic, Carboniferous,

Cross-bedded sandstone (Cjf),

 

Mesozoic, Cretaceous,

Cross-bedded sandstone (Ksl), and kaolinitic sandstone (Kbj) at Wadi Jabjabah

 

Cenozoic-, Tertiary,

altered sub-volcanic dacite with pyrite gold mineralisation (Tsvd), (Umm Qurayat)

 

Quaternary

wadi alluvium (Qa)