Geological Setting and Mineralization of Gicik Low-sulfidation Epithermal Au-Ag±Te Deposit (Ankara, North-Central Anatolia)

Geological Features of the Chromite Deposits in Tunceli Province Önal, Ali; Aktağ, Alican; Toksoy Köksal, Fatma; Çimen, Okay; Öztüfekçi-önal, Ayten (null; 2015-09-11)
Geological Features of the Chromite Deposits in Tunceli Province Turkey Önal, Ali; Aktağ, Alican; Köksal, Fatma; Çimen, Okay; Öztüfekçi Önal, Ayten (2015-09-11)
GEOLOGICAL HISTORY OF THE NORTHWARD ARCHED SEGMENT OF THE NORTH ANATOLIAN TRANSFORM-FAULT ZONE DIRIK, K (Wiley; 1993-12-01) The study area is located in the southern part of the Central Pontides. The rocks exposed in this region have been divided into three major groups: basement, cover sequence and volcanic rocks. The basement rocks are composed of metamorphic units and a chaotic assemblage derived from an accretionary prism produced during the northward subduction of northern Neo-Tethys during the Late Cretaceous. During the same period, the basal element of the cover sequence, a thick and coarsening upward flysch succession (...
Geological evolution of the gediz graben, sw turkey: temporal and spatial variation of the graben Çiftçi, Bozkurt N; Bozkurt, Erdin; Department of Geological Engineering (2007) Gediz Graben is a continental extensional basin filled with Neogene sediments. Its margins are controlled by active ~EW-trending fault systems with major system, in terms of total offset and duration of activity, located along the southern margin. The graben evolved as a half graben by the activity of the southern margin during the entire Miocene. Then, the northern margin-bounding structure initiated by PlioQuaternary to form the current configuration of the graben with an inherited asymmetry. The southern...
Sedimentary records of past earthquakes in Boraboy Lake during the last ca 600 years (North Anatolian Fault, Turkey) Avşar, Ulaş; De Batıst, Marc; Schmidt, Sabine; Fagel, Nathalie (2015-09-01) Multiproxy sedimentological analyses along 4.9 m-long sequence of Boraboy Lake, which is located on the central eastern part of the North Anatolian Fault (NAF), reveal the sedimentary traces of past large earthquakes in the region. The lake has a relatively large catchment area (10 km(2)) compared to its size (0.12 km(2)), which renders sedimentation sensitive to heavy rain/storm events. Accordingly, the background sedimentation, which is composed of faintly laminated reddish/yellowish brown clayey silt, is...

Citation Formats

A. Çil and A. İmer, “Geological Setting and Mineralization of Gicik Low-sulfidation Epithermal Au-Ag±Te Deposit (Ankara, North-Central Anatolia),” presented at the Sustainable Mineral Resources Supply: Challenges for Future Generations, Cenevre, İsviçre, 2022, Accessed: 00, 2022. [Online]. Available: https://secureservercdn.net/160.153.138.203/f7y.24c.myftpupload.com/wp-content/uploads/2022/09/SMRS2022_AbstractBook_V2.pdf.