Insights into biaxial extensional tectonics: an example from the Sandikli Graben, West Anatolia, Turkey
Cihan, Mustafa, Saraç, Gerçek, and Gökçe, Oktay (2003) Insights into biaxial extensional tectonics: an example from the Sandikli Graben, West Anatolia, Turkey. Geological Journal, 38 (1). pp. 47-66.
|PDF (Published Version) - Repository staff only - Requires a PDF viewer such as GSview, Xpdf or Adobe Acrobat Reader|
View at Publisher Website: http://dx.doi.org/10.1002/gj.928
West Anatolia, together with the Aegean Sea and the easternmost part of Europe, is one of the best examples of continental extensional tectonics. It is a complex area bounded by the Aegean–Cyprus Arc to the south and the North Anatolian Fault Zone (NAFZ) to the north. Within this complex and enigmatic framework, the Sandıklı Graben (10 km wide, 30 km long) has formed at the eastern continuation of the Western Anatolian extensional province at the north-northwestward edge of the Isparta Angle. Recent studies have suggested that the horst–graben structures in West Anatolia formed in two distinct extensional phases. According to this model the first phase of extension commenced in the Early–Middle Miocene and the last, which is accepted as the onset of neotectonic regime, in Early Pliocene. However, it is controversial whether two-phase extension was separated by a short period of erosion or compression during Late Miocene–Early Pliocene. Both field observations and kinematic analysis imply that the Sandıklı Graben has existed since the Late Pliocene, with biaxial extension on its margins which does not necessarily indicate rotation of regional stress distribution in time. Although the graben formed later in the neotectonic period, the commencement of extension in the area could be Early Pliocene (c. 5 Ma) following a severe but short time of erosion at the end of Late Miocene. The onset of the extensional regime might be due to the initiation of westward motion of Anatolian Platelet along the NAFZ that could be triggered by the higher rate of subduction at the east Aegean–Cyprus Arc in the south of the Aegean Sea.
|Item Type:||Article (Refereed Research - C1)|
|Keywords:||Sandıklı Graben; Anatolia; neotectonics; biaxial extension; Miocene; Pliocene|
|FoR Codes:||04 EARTH SCIENCES > 0403 Geology > 040313 Tectonics @ 100%|
|SEO Codes:||97 EXPANDING KNOWLEDGE > 970104 Expanding Knowledge in the Earth Sciences @ 100%|
|Deposited On:||03 Nov 2010 11:34|
|Last Modified:||18 Oct 2013 01:07|
Last 12 Months: 0
|Citation Counts with External Providers:|
Repository Staff Only: item control page