Abstract: One of the largest interior basins in Turkey, the Tuzgölü Basin related with the Haymana and Kırıkkale Basins, has smooth topography, a stable young sedimentary cover and limited outcrop zones. But the study area bears a complex geology with intensive tectonism and poor seismic data quality beneath the surface. The complexity of the subsurface geology was attempted to be solved and important structural components giving evident anomalies were determined using the gravity and magnetic methods in integration with each other. Most important determination from the gravity anomaly map is the existence of a large and unique basin (named as Tuzgölü Basin in this study) in the south of Tuzgölü, in spite of separate classification as Tuzg...
The central Anatolia comprises various continental fragments belonging to Laurasia at the north and ...
The Suşehri section of the North Anatolian Fault Zone (NAFZ) is dominated by an active fault-wedge b...
The Erzurum-Horasan-Pasinler basin, which surrounds Miocene rocks, is oriented approximately E–W and...
ABSTRACT: In this study, all available geological, geophysical and geo-chemical data were integrated...
Abstract: Some 100 km southwest of Tuz Lake in central Turkey there are strong gravity and magnetic ...
Abstract: The geology of the Çankırı Basin has been studied using multi-source data including satell...
Abstract: This study was carried out in the Pasinler-Horasan basin (Eastern Turkey), where sedimenta...
The central Anatolia is comprises successor basins developed at the terminal phase of closure of Neo...
Abstract: Th e North Anatolian Fault System (NAFS) that separates the Eurasian plate in the north fr...
The Tuz Gölü Basin is the largest sedimentary depression located at the center of the Central Anatol...
Detection of the linear features is a useful task to understand the tectonism of a region. Gravity a...
SUMMARY. — The Tuz Gölü basin is a NW-SE trending intramontane basin situated in a transverse struct...
The Miocene Central Anatolian Orogenic Plateau (CAP) is a semi-arid nearly-flat elevated terrain fla...
The Cappadocia region, located in Central Turkey, is characterized by widespread lava flows and volc...
Abstract: The Cumaovası basin, formerly known as the Çubukludağ Graben, is located at the western en...
The central Anatolia comprises various continental fragments belonging to Laurasia at the north and ...
The Suşehri section of the North Anatolian Fault Zone (NAFZ) is dominated by an active fault-wedge b...
The Erzurum-Horasan-Pasinler basin, which surrounds Miocene rocks, is oriented approximately E–W and...
ABSTRACT: In this study, all available geological, geophysical and geo-chemical data were integrated...
Abstract: Some 100 km southwest of Tuz Lake in central Turkey there are strong gravity and magnetic ...
Abstract: The geology of the Çankırı Basin has been studied using multi-source data including satell...
Abstract: This study was carried out in the Pasinler-Horasan basin (Eastern Turkey), where sedimenta...
The central Anatolia is comprises successor basins developed at the terminal phase of closure of Neo...
Abstract: Th e North Anatolian Fault System (NAFS) that separates the Eurasian plate in the north fr...
The Tuz Gölü Basin is the largest sedimentary depression located at the center of the Central Anatol...
Detection of the linear features is a useful task to understand the tectonism of a region. Gravity a...
SUMMARY. — The Tuz Gölü basin is a NW-SE trending intramontane basin situated in a transverse struct...
The Miocene Central Anatolian Orogenic Plateau (CAP) is a semi-arid nearly-flat elevated terrain fla...
The Cappadocia region, located in Central Turkey, is characterized by widespread lava flows and volc...
Abstract: The Cumaovası basin, formerly known as the Çubukludağ Graben, is located at the western en...
The central Anatolia comprises various continental fragments belonging to Laurasia at the north and ...
The Suşehri section of the North Anatolian Fault Zone (NAFZ) is dominated by an active fault-wedge b...
The Erzurum-Horasan-Pasinler basin, which surrounds Miocene rocks, is oriented approximately E–W and...