2 4 2 | chives : 2 . A * . . ; . . 
| 2004 International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part B7. Istanbul 2004 
2 to 10 
  
34 100€ 34'200'E MOTE 
  
tite and 
e rocks 25-500" 
having 
s in the 
of the 
) 50 c/s 
    
    
  
    
      
25'4007N A38 * 4 x ; d 25° 4008 
merous 
lineated 
1 alkali 
Abu El 
eadings 
1 175 to 
25 300"N 
  
  
  
  
  
  
tite and ON 5 uU. 5 à Klometers 
^. veins 
lineated Figure 1: U» 30 and U/Th » 10 (red) distribution and intensity map superimposed on 
felsitic 
| Nusla 
rites are 
U and 
ge from 
Landsat TM image of the study area 
  
34'200"E 
L 
  
orded at 
northern 25500N] 4.2 
lug cuts à 
clastic- 
; of the 
F25'50Q"N 
' veins: mee 
25400 NT x « H25'400"N 
     
    
    
   
      
  
  
  
  
  
  
  
  
  
    
  
  
  
Xf Gabal irse al US 
ee i eh mess Vari wx Re 
ns reach N) : N "rem T NEES xQ; Et-Shush 
- x N x w eb z x x x 
of the x a d NN IR 
Fo FR Omani XT 
irements E § ANN 
. NG C 
its of. U NN 
. . > N 
limit of N 
NN 
PAS AN 
Legend 
«| Granodiorite ECT Dawi Formation ; e Left lateral strike-siip fault —je Syntorm 
.| Gabtxo-diorite rocks Bl 72vo oo: i: Plio-Plestocene Qaternary — Normal faut $9 Antiform 
XN = vy -- nl 
AXWS Acidic metavolcanics = Quatrz plugs y V v Meódie toUpper Miocene S. ered faut 
; X + ERES Gahsl ELR 7 ion iis Infered Loft lateral strike-slip fault 
XC sic meto) rz oz M (te gri ES Ga ossas Forma 
2 AN Basic metovolcanics luscovite grante : La. tréorod Tiynret fault 
1777] Metavolcanosedimentary rocks B 111 Red granite Lower Miocene 
du 
(XXX Serpentinte rocks 
     
   
adh. Thrust fault 
—— Concoaled fault 
-Ë Hammamat sediments 
a 10 5 0 10 Kilometers 
  
  
  
  
Ophioktic melange e . . x d Biotite grano : Dakhla Formation 
ne 
  
  
  
Figure. 2. Geological mab of the studv area. modified after EGSMA 1992. 
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