Full text: Proceedings, XXth congress (Part 7)

  
  
  
  
International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part B7. Istanbul 2004 
Conclusions 
Tectonically, Sivas Basin has been developed on the Alpine- 
Himalayan belt with the complex interactions of Eurasian, 
Arabian and African plates. Remarkable marks of this 
collisional process were observed roughly in N-S direction 
within the Oligocene Hafik formation, which was composed of 
mainly massive gypsum deposits after Upper Miocene. 
Deformational behaviour of décollement levels are proofed the 
presence of thin-skinned deformation along their contacts 
within horizontally Mio-Pliocene sediments. 
Brovey transform, which was also known a useful image fusion 
method, may be very useful spatially in lithological 
differentiation studies combining with panchromatic band in 
Landsat ETM+ images. On the other hand, public use digital 
elevation data such as SRTM-3 and their evaluations in planar 
and three-dimensional modes aid structural evaluation efforts in 
geosciences and clench the results of directional edge 
enhancement processes. 
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Acknowledgements 
The author would like to express special thanks to NIK 
Construction Trade Co./Turkey and ER  Mapper/England 
authorities for supporting. 
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