The geometry, deformation mechanism and kinematics of the Sürgü Fault Zone is investigated by using remotely sensed data including Landsat TM and ASTER imagery combined with SRTM, and stereo-aerial photographs. They are used to extract information related to regional lineaments and tectono-morphological characteristics of the SFZ. Various image processing and enhancement techniques including contrast enhancement, PCA, DS and color composites are applied on the imagery and three different approaches including manual, semi automatic and automatic lineament extraction methods are followed. Then the lineaments obtained from ASTER and Landsat imagery using manual and automatic methods are overlaid to produce a final lineaments map. The results h...
In the Zagros structural zone of Iran, there is a broad range of emergent salt domes, a unique morph...
The Korucu-Dugla study area (225 km(2)) located in western Turkey was selected for the application o...
AbstractAntakya-Kahramanmaraş depression has nearly 180 – 200km length and 5 – 40km width. Research ...
The Surgu Fault Zone (SFZ) is located in SE Anatolia extending from Goksun in the west to Celikhan i...
The purposes of this study are to extract lineaments from satellite images in order to contribute to...
Tectonic movements which took place in Late Cretaceous-Neogene time interval make the geology of Cen...
The Gaziköy–Saros region is located in the western part of the North Anatolian Fault Zone (NAFZ), Tu...
The goal of this project is to compile and interpret remotely sensed imagery and produce maps intend...
Fault displacements are being measured by geological observations using the method of detecting and ...
Syste'm Pour l‘Observation de la Terre (SPOT) remote sensing satellite data have useful characterist...
The assessment of earthquake hazards and mineral and oil potential of a given region requires a deta...
In current paper, geometrical relationship between the longitudinal faults of a zone of the folded Z...
Landsat TM and ASTER data were used in the neotectonics study of Western Mongolia. The latter has be...
The 22 August 1902 Mw 7.7 Atushi earthquake is the most disastrous seismic event in the southwestern...
On Friday, January 24, 2020 at 20.55:11 local time (17:55 UTC), an earthquake with a magnitude of Mw...
In the Zagros structural zone of Iran, there is a broad range of emergent salt domes, a unique morph...
The Korucu-Dugla study area (225 km(2)) located in western Turkey was selected for the application o...
AbstractAntakya-Kahramanmaraş depression has nearly 180 – 200km length and 5 – 40km width. Research ...
The Surgu Fault Zone (SFZ) is located in SE Anatolia extending from Goksun in the west to Celikhan i...
The purposes of this study are to extract lineaments from satellite images in order to contribute to...
Tectonic movements which took place in Late Cretaceous-Neogene time interval make the geology of Cen...
The Gaziköy–Saros region is located in the western part of the North Anatolian Fault Zone (NAFZ), Tu...
The goal of this project is to compile and interpret remotely sensed imagery and produce maps intend...
Fault displacements are being measured by geological observations using the method of detecting and ...
Syste'm Pour l‘Observation de la Terre (SPOT) remote sensing satellite data have useful characterist...
The assessment of earthquake hazards and mineral and oil potential of a given region requires a deta...
In current paper, geometrical relationship between the longitudinal faults of a zone of the folded Z...
Landsat TM and ASTER data were used in the neotectonics study of Western Mongolia. The latter has be...
The 22 August 1902 Mw 7.7 Atushi earthquake is the most disastrous seismic event in the southwestern...
On Friday, January 24, 2020 at 20.55:11 local time (17:55 UTC), an earthquake with a magnitude of Mw...
In the Zagros structural zone of Iran, there is a broad range of emergent salt domes, a unique morph...
The Korucu-Dugla study area (225 km(2)) located in western Turkey was selected for the application o...
AbstractAntakya-Kahramanmaraş depression has nearly 180 – 200km length and 5 – 40km width. Research ...