Year 1989, Volume 109, Issue 109, Pages 1 - 16 1989-02-01

DENİZLİ'NİN GÜNEYİNDE MENDERES MASİFİ VE LİKYA NAPLARININ JEOLOJİSİ
Geology of the Menderes Massif and the Lycian Nappes South of Denizli, Western Taurides

Aral İ. OKAY [1]

175 1027

Honaz dağı bölgesi üst üste duran tektonik birimlerden oluşmuştur. Batıda, bu tektonik istifin en altında monoton yeşil metaşeylden oluşan yaşı belirsiz Honaz şeyli yer alır. Honaz şeylinin üzerinde tektonik bir dokanakla masif beyaz kireçtaşı ve ince tabakalı çörtlü kireçtaşı ve şeylden oluşan, hafif bir metamorfizma geçirmiş, Menderes masifinin Mesozoyik örtü birimi yer alır. Menderes masifi üzerinde tektonik dokanakla Likya naplarına ait Sandak birimi bulunur. Mesozoyik yaşta dolomit ve kireçtaşından oluşan Sandak biriminin üzerinde ise ofiyolit yer almaktadır. Bütün bu birimler Honaz antiklinali diye adlandırılan, doğuya devrik büyük bir antiklinal oluşturur; Honaz antiklinalinin devrik kanadı altında, tektonik bir dokanakla, Göbecik tepe birimi adı verilen Geç Kretase - Orta/Geç Eosen yaşta pelajik bir sedimanter istif yer almaktadır. Göbecik tepe birimi Honaz dağı bölgesinde nispî otokton birimi teşkil etmektedir. Honaz dağı bölgesindeki birimlerde Geç Kretase, Orta Eosen ve Geç Eosen/Oligosen tektoniğinin izi görülür. Ofiyolitin, Sandak birimi üzerine yerleşmesi muhtemelen Geç Kretasede olmuş, Sandak biriminin Menderes masifi üzerine bindirmesi muhtemelen Orta Eosende, tüm bu birimlerin Göbecik tepe birimi üzerine yerleşmesi ve Honaz antiklinalinin oluşması Geç Eosen/Oligosende meydana gelmiştir.

Mount Honaz region in the Western Taurides is made up of superimposed several tectonic units. In the west, monotonous green metashales called the Honaz shale occur at the base of the tectonic stack. Honaz shale is tectonically overlain by weakly metamorphosed, massif white limestone, thinly bedded cherty limestone and shale which covers the Mendercs massif. Menderes massif is in turn tectonically overlain by the Sandak complex of the Lycian nappes made up of Mesozoic dolomites and limestones and ophiolite mainly of harzburgite lies oven the Sandak complex. All these tectonic units form an eastward overturned major anticline called the Honaz anticline; a pelagic sedimentary sequence of Late Cretaceous—Middle/Late Eocene age, called the Göbecik Tepe complex, occurs tectonically beneath the overturned limb of the Honaz anticline. The Göbecik Tepe complex constitutes the relative autochthonous in the region of the Mount Honaz. Different tectonic units in the Mount Honaz region show effects of Late Cretaceous, Middle Eocene and Late Eocene/Oligocene tectonics. Obduction of the ophiolite over the Sandak complex probably occurred during the Late Cretaceous, while the age of thrusting of the Sandak complex over the Menderes massif is probably Middle Eocene. Emplacement of these tectonic units over the Göbecik Tepe complex and the formation of the Honaz anticline is of Late Eocene/Oligocene age. 

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Primary Language en
Subjects Engineering
Journal Section Articles
Authors

Author: Aral İ. OKAY (Primary Author)

Bibtex @research article { bulletinofmre52265, journal = {Bulletin of the Mineral Research and Exploration}, issn = {0026-4563}, eissn = {2651-3048}, address = {Maden Tetkik Arama Genel Müdürlüğü}, year = {1989}, volume = {109}, pages = {1 - 16}, doi = {}, title = {Geology of the Menderes Massif and the Lycian Nappes South of Denizli, Western Taurides}, key = {cite}, author = {OKAY, Aral İ.} }
APA OKAY, A . (1989). Geology of the Menderes Massif and the Lycian Nappes South of Denizli, Western Taurides. Bulletin of the Mineral Research and Exploration, 109 (109), 1-16. Retrieved from http://dergipark.org.tr/bulletinofmre/issue/3928/52265?publisher=mta
MLA OKAY, A . "Geology of the Menderes Massif and the Lycian Nappes South of Denizli, Western Taurides". Bulletin of the Mineral Research and Exploration 109 (1989): 1-16 <http://dergipark.org.tr/bulletinofmre/issue/3928/52265?publisher=mta>
Chicago OKAY, A . "Geology of the Menderes Massif and the Lycian Nappes South of Denizli, Western Taurides". Bulletin of the Mineral Research and Exploration 109 (1989): 1-16
RIS TY - JOUR T1 - Geology of the Menderes Massif and the Lycian Nappes South of Denizli, Western Taurides AU - Aral İ. OKAY Y1 - 1989 PY - 1989 N1 - DO - T2 - Bulletin of the Mineral Research and Exploration JF - Journal JO - JOR SP - 1 EP - 16 VL - 109 IS - 109 SN - 0026-4563-2651-3048 M3 - UR - Y2 - 2019 ER -
EndNote %0 Bulletin of the Mineral Research and Exploration Geology of the Menderes Massif and the Lycian Nappes South of Denizli, Western Taurides %A Aral İ. OKAY %T Geology of the Menderes Massif and the Lycian Nappes South of Denizli, Western Taurides %D 1989 %J Bulletin of the Mineral Research and Exploration %P 0026-4563-2651-3048 %V 109 %N 109 %R %U
ISNAD OKAY, Aral İ. . "Geology of the Menderes Massif and the Lycian Nappes South of Denizli, Western Taurides". Bulletin of the Mineral Research and Exploration 109 / 109 (February 1989): 1-16.