Add to ORKGThe Cumaovasi basin, formerly known as the Cubukludag Graben, is located at the western end of Gediz and Kucuk Menderes grabens in the west Anatolian extensional province. It is 5-17-km wide and 35-km-long, NNE-SSW-trending, asymmetric basin that was formed under the control of strike-slip and oblique-slip normal faults
The origin of NE-trending basins and their relation to the E-W-trending grabens in western Turkey ha...
The Suşehri section of the North Anatolian Fault Zone (NAFZ) is dominated by an active fault-wedge b...
Denizli basin is situated at the junction of NW-SE trending Gediz Graben and E-W trending Buyuk Mend...
Abstract: The Cumaovası basin, formerly known as the Çubukludağ Graben, is located at the western en...
The Kiraz Basin which is located at the eastern end of the Kucuk Menderes Graben was previously cons...
Abstract: Th e North Anatolian Fault System (NAFS) that separates the Eurasian plate in the north fr...
The study area is a strike-slip basin of approximately 1-9 km wide, 66 km long and N65 degrees W tre...
Study area, the Yeniçaga Basin, is located in the western part of the North Anatolian Fault System. ...
Integrated study on the stratigraphic and structural features of the Soke Basin on the western end o...
The East Anatolian fault system (EAFS) is the 80-km-wide, 700-km-long, NE-trending sinistral strike-...
The Esen Basin of southwestern Anatolia formed as a NE-trending intramontane extensional graben, ca....
The Hazar Basin is a 25 km-long, 7 km-wide and 216m-deep depression located on the central section o...
The Hazar Basin is a 25 km-long, 7 km-wide and 216 m-deep depression located on the central section ...
The Denizli graben-horst system (DGHS) is located at the eastern-southeastern converging tips of thr...
The Kocacay Basin (KCB) is a key area in western Anatolia - a well-known extended terrane where regi...
The origin of NE-trending basins and their relation to the E-W-trending grabens in western Turkey ha...
The Suşehri section of the North Anatolian Fault Zone (NAFZ) is dominated by an active fault-wedge b...
Denizli basin is situated at the junction of NW-SE trending Gediz Graben and E-W trending Buyuk Mend...
Abstract: The Cumaovası basin, formerly known as the Çubukludağ Graben, is located at the western en...
The Kiraz Basin which is located at the eastern end of the Kucuk Menderes Graben was previously cons...
Abstract: Th e North Anatolian Fault System (NAFS) that separates the Eurasian plate in the north fr...
The study area is a strike-slip basin of approximately 1-9 km wide, 66 km long and N65 degrees W tre...
Study area, the Yeniçaga Basin, is located in the western part of the North Anatolian Fault System. ...
Integrated study on the stratigraphic and structural features of the Soke Basin on the western end o...
The East Anatolian fault system (EAFS) is the 80-km-wide, 700-km-long, NE-trending sinistral strike-...
The Esen Basin of southwestern Anatolia formed as a NE-trending intramontane extensional graben, ca....
The Hazar Basin is a 25 km-long, 7 km-wide and 216m-deep depression located on the central section o...
The Hazar Basin is a 25 km-long, 7 km-wide and 216 m-deep depression located on the central section ...
The Denizli graben-horst system (DGHS) is located at the eastern-southeastern converging tips of thr...
The Kocacay Basin (KCB) is a key area in western Anatolia - a well-known extended terrane where regi...
The origin of NE-trending basins and their relation to the E-W-trending grabens in western Turkey ha...
The Suşehri section of the North Anatolian Fault Zone (NAFZ) is dominated by an active fault-wedge b...
Denizli basin is situated at the junction of NW-SE trending Gediz Graben and E-W trending Buyuk Mend...