NEOTECTONIC FEATURES OF THE CAVUSCUGOL GRABEN (CENTRAL ANATOLIA, TURKEY)
Küçük Resim Yok
Tarih
2008
Yazarlar
Dergi Başlığı
Dergi ISSN
Cilt Başlığı
Yayıncı
INT SCIENTIFIC CONFERENCE SGEM
Erişim Hakkı
info:eu-repo/semantics/closedAccess
Özet
The aim of this study is to elucidate the neotectonic characteristics of the Cavuscugol graben. The Cavuscugol graben is 3-8 km wide 28 km long. It is a N-S trending actively evolving extensional structure containing infills of fluvial sediments of Pliocene-Quaternary age. The Cavuscugol graben is bounded on both sides by oblique-slip normal faults. These faults trend N-S and named as Ilgin Fault on the west and Tekeler Fault on the east. The footwall side of the faults are composed of the pre-Late Cretaceous metamorphic rocks and the Miocene-Pliocene fluviolacustrine sediments. Field studies indicated that the graben has been developed as a result of E-W extension since Upper Pliocene.
Açıklama
8th International Scientific Conference on Modern Management of Mine Producing, Geology and Environmental Protection -- JUN 16-20, 2008 -- Sofia, BULGARIA
Anahtar Kelimeler
Cavuscugol graben, neotectonic, oblique-slip normal faults, Central Anatolia
Kaynak
SGEM 2008: 8TH INTERNATIONAL SCIENTIFIC CONFERENCE, VOL I, CONFERENCE PROCEEDINGS: MODERN MANAGEMENT OF MINE PRODUCING GEOLOGY AND ENVIRONMENTAL PROTECTION
WoS Q Değeri
N/A
Scopus Q Değeri
N/A
