气候变化领域集成服务门户(CCPortal): Late Cenozoic tectono-sedimentary evolution of the Ulukışla Basin: progressive basin development in south-central Turkey

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DOI	10.1007/s00531-019-01805-8
	Late Cenozoic tectono-sedimentary evolution of the Ulukışla Basin: progressive basin development in south-central Turkey
	Gürbüz E.; Seyitoğlu G.; Güney A.
发表日期	2020
ISSN	14373254
起始页码	345
结束页码	371
卷号	109 期号:1
英文摘要	The Ulukışla Basin is one of the most important late Cretaceous-Cenozoic basins in central Anatolia. The basin is surrounded by the Bolkar Mountains of Tauride Platform in the south, the Niğde Massif of Central Anatolian Crystalline Complex to the north, and the Ecemiş Fault Zone and Aladağ Mountains in the east. The fact that time interval proposed for the formation of Ulukışla Basin is quite wide and more than one tectonic regime prevailed in the region, have led to various suggestions concerning the evolution of the basin. While the suggestions majorly examine the character of the basin during the late Cretaceous-early Cenozoic, the number of detailed studies on the status of the basin in the late Cenozoic is limited. In this study, we focused on the less-studied late Cenozoic evolution to differentiate the tectonic phases that controlled the development of Ulukışla Basin through structural data, and elaborate the responses of sedimentation and paleogeography during this period through detailed facies analyses. Our findings indicate that the Ulukışla Basin, which started to develop as a supradetachment basin in the late Cretaceous, has continued its extensional development progressively during its Cenozoic history. While the relatively well-studied early Cenozoic sequences represent a marine environment that was rapidly changed shallow- to deep-sea environment and then gained a shallow character by the middle Eocene, sedimentary features and fossil contents of the late Cenozoic units characterize deposition started in a paralic environment changing into a terrestrial environment rapidly, as a result of isolation by the uplifting of surrounding topographies while the basin continues its development under an extensional tectonic regime. However, the extensional basin history surceased in post-middle Eocene and post-middle Miocene, probably caused by the closing processes of the different branches of Neotethys Ocean. © 2020, Geologische Vereinigung e.V. (GV).
英文关键词	Central Anatolia; Depositional environments; Extensional tectonics; Paleogeography; Taurides
语种	英语
scopus关键词	basin evolution; Cenozoic; depositional environment; Eocene; extensional tectonics; marine environment; Miocene; paleogeography; sedimentary basin; Anatolia; Bolkar Mountains; Taurides; Turkey
来源期刊	International Journal of Earth Sciences
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/147724
作者单位	Aksaray Üniversitesi, Mühendislik Fakültesi Harita, Mühendisliği Bölümü, Aksaray, 68100, Turkey; Ankara Üniversitesi, Mühendislik Fakültesi, Jeoloji Mühendisliği Bölümü, Tektonik Araştırma Grubu, Gölbaşı, Ankara 06830, Turkey; Aksaray Üniversitesi, Mühendislik Fakültesi, Jeoloji Mühendisliği Bölümü, Aksaray, 68100, Turkey
推荐引用方式 GB/T 7714	Gürbüz E.,Seyitoğlu G.,Güney A.. Late Cenozoic tectono-sedimentary evolution of the Ulukışla Basin: progressive basin development in south-central Turkey[J],2020,109(1).
APA	Gürbüz E.,Seyitoğlu G.,&Güney A..(2020).Late Cenozoic tectono-sedimentary evolution of the Ulukışla Basin: progressive basin development in south-central Turkey.International Journal of Earth Sciences,109(1).
MLA	Gürbüz E.,et al."Late Cenozoic tectono-sedimentary evolution of the Ulukışla Basin: progressive basin development in south-central Turkey".International Journal of Earth Sciences 109.1(2020).