recognilion 
lls were 
[tes of 
ration 
! vocks 
sis 
gray scale 
M hioul a 
ies and 
ogical unils. 
isfaclory on 
(08 mountain 
Zones in 
id nearly N-S 
i timage às 
te west. The 
Ss ih the east. 
(Yes are in N-S 
due lo the 
uves olheı 
pus in Ihe 
hus 
l'acepl Jo) 
any mappable 
'he evisling 
open useful 
Eh, 7 via 
fee led 
witday res of 
Ogvuphs is 
  
   
   
  
  
  
   
  
  
  
  
  
  
   
  
  
  
  
  
  
  
  
  
  
   
   
    
     
   
too small and the Landsat imagery has a resolution of 8) meters. the 
observations were only based on interprelations of bholographs wilhoul 
magnifying instruments excepl for the hand lens. No new dula were found 
to reinforce the dala previously known. 
The observations of structural lineaments were quite successful. Il 
is possible lo oblain some dala lo be used for the vegional analyses by 
means of the fracture lvace analysis. Bul lhe primary objeclive of lhe 
exploration for oil is to study of geological structures, lhevefove this 
approach mighl seen inadequale. However, more sophislicaled 
techniques should improve this interpretation. 
Acknowledgements 
The author wishes lo express his thanks to the General Directorate 
of the Turkish Petroleum Corp. (TPAO) for permiting lo submil {his paper 
and lhe Central Treaty Ovganizalion (CENTO) for supplying lhe Landsal 
images. 
  
[ Y 
‘ROMANIA ) 
YUGOSLAVIA Ny 
7 Sa 7" 
     
    
  
    
    
n UNION M 
BLACK SE A N 
ol 
fn Ni sea TL 
; V 
oF 
TURKEY t 2 { 
Bon 3 
SS S S 
MEDITERRANEAN SEA 
Là Ce syria. À 
AN LEBANO / "P f IRAN 
= : A + 
KL ISRAEL | Ÿ nt d IRA b 
EGYPT C : C EN K > 
N. ) 
  
  
| 20 V JORDAN ! 
— 3d — QJ ÁÀ ds X EE 
SAUDI ARABIA^—- —. 7. (ere. 
STUDY AREA. A