The Denizli Basin (southwestern Anatolia, Turkey) contains a record of environmental changes dating since the Early Miocene. Detailed facies analysis of the Neogene formations in this half-graben enables us to document successive depositional regimes and palaeogeographic settings. Sedimentation commenced in the Early Miocene with the deposition of alluvial-fan and fluvial facies (Kizilburun Formation). At this stage, alluvial fans sourced from elevated areas to the south prograded towards the basin centre. The Middle Miocene time saw the establishment of marginal lacustrine and wetland environments followed by the development of a shallow lake (Sazak Formation). The uppermost part of this unit consists of evaporitic saline lake and saline m...
The Late Miocene lacustrine Aci{dotless}göl Basin, SW Turkey, formed as an orogen-top, extensional h...
The NW-trending Denizli basin of the SW Turkey is one of the neotectonic grabens in the Aegean exten...
The Akkaşdaǧι area, situated in the southern margin of the Tertiary Çankιrι-Çorum Basin, Central Ana...
The Denizli Basin (southwestern Anatolia, Turkey) contains a record of environmental changes dating ...
The Denizli Basin (southwestern Anatolia, Turkey) contains a record of environmental changes dating ...
The extensional intramontane grabens that formed in southwestern Anatolia in the Late Cenozoic bear ...
The neotectonic development of western Anatolia was characterized by the formation of numerous grabe...
The late Cenozoic extensional deformation formed several NE-trending fluvio-lacustrine basins in SW ...
The Eşen Basin of southwestern Anatolia formed as a NE-trending intramontane extensional graben, ca....
The neotectonic development of western Anatolia was characterized by the formation of numerous grabe...
The extensional intramontane grabens that formed in southwestern Anatolia in the Late Cenozoic bear ...
The Akkasdagi area, situated in the southern margin of the Tertiary Cankiri- Corum Basin, Central An...
The Gediz Graben is a continental extensional basin filled with Miocene to Recent sediments. The evo...
The Karakecili basin is an intermontane basin located about 60 km SE of Ankara in central Turkey and...
The late Cenozoic extensional deformation formed several NE-trending fluvio-lacustrine basins in SW ...
The Late Miocene lacustrine Aci{dotless}göl Basin, SW Turkey, formed as an orogen-top, extensional h...
The NW-trending Denizli basin of the SW Turkey is one of the neotectonic grabens in the Aegean exten...
The Akkaşdaǧι area, situated in the southern margin of the Tertiary Çankιrι-Çorum Basin, Central Ana...
The Denizli Basin (southwestern Anatolia, Turkey) contains a record of environmental changes dating ...
The Denizli Basin (southwestern Anatolia, Turkey) contains a record of environmental changes dating ...
The extensional intramontane grabens that formed in southwestern Anatolia in the Late Cenozoic bear ...
The neotectonic development of western Anatolia was characterized by the formation of numerous grabe...
The late Cenozoic extensional deformation formed several NE-trending fluvio-lacustrine basins in SW ...
The Eşen Basin of southwestern Anatolia formed as a NE-trending intramontane extensional graben, ca....
The neotectonic development of western Anatolia was characterized by the formation of numerous grabe...
The extensional intramontane grabens that formed in southwestern Anatolia in the Late Cenozoic bear ...
The Akkasdagi area, situated in the southern margin of the Tertiary Cankiri- Corum Basin, Central An...
The Gediz Graben is a continental extensional basin filled with Miocene to Recent sediments. The evo...
The Karakecili basin is an intermontane basin located about 60 km SE of Ankara in central Turkey and...
The late Cenozoic extensional deformation formed several NE-trending fluvio-lacustrine basins in SW ...
The Late Miocene lacustrine Aci{dotless}göl Basin, SW Turkey, formed as an orogen-top, extensional h...
The NW-trending Denizli basin of the SW Turkey is one of the neotectonic grabens in the Aegean exten...
The Akkaşdaǧι area, situated in the southern margin of the Tertiary Çankιrι-Çorum Basin, Central Ana...