Results 51 to 60 of about 239 (95)
İzmirin kuzeydoğusunda yeralan Akhisar çevresinde alttan üste Menderes masifi, Likya napları ve İzmir-Ankara zonuna ait Bornova melanjı ana tektonik kuşakları oluşturur. Menderes masifi bu alanda masif mermerler ile temsil edilmektedir. Likya naplarına ait Akhisar napı bu çalışmada yeni tanımlanmıştır ve altta riyolit, çakıltaşı arakatkıları ve ...
openaire +1 more source
Late Cenozoic Sedimentary Evolution of the Antalya Basin, Southern Turkey
International audienceThe Late Cenozoic Antalya Basin developed unconformably on a foundered basement comprising Mesozoic autochthonous carbonate platform(s) overthrust by the Lycian Nappes, the Antalya Nappes and the Alanya Massif metamorphics within ...
Ciner, A. +4 more
core +1 more source
Middle Pleistocene tectonic events around the SE Aegean Sea: Insights from magnetostratigraphy, (U-Th)/He zircon dating, and fault kinematics in the Datça Graben (SW Türkiye). [PDF]
İnce MD +7 more
europepmc +1 more source
ELMALI (ANTALYA, BATI TOROSLAR) KUZEYGNDE LGKYA NAPLARININ JEOLOJG
The study area comprises the area between HacÍyusuflar, BayÍndÍr and Gkizler villagesnorth of ElmalÍ (Antalya), Western Taurides, and includes different tectonic units with characteristicstratigraphic, lihologic and structural features.
AKSARI, Süleyman, AKSOY, Rahmi
core
The Bornova Flysch Zone consists of large blocks of Mesozoic limestone, basalt, serpentinite and radiolarian chert in a highly sheared clastic matrix of latest Cretaceous to Paleocene age.
Altıner, Demir, Okay, Aral I.
core
The metamorphic basement consists of the following lithologies in ascending order: sillimanite-garnet gneiss, sillimanite-garnet-kyanite schist, sillimanite-staurolite-garnet-kyanite schist, staurolite-garnet schist and garnet mica schist.
Mark, T.D. +4 more
core
Mesoscopic and microscopic structures along the contact between Menderes massif and Lycian nappes
openaire +1 more source
The orientation, asymmetry and cross-cutting relationships of the structures along the contact zone between the Lycian nappes and the Menderes Massif suggest the presence of three deformation phases in the Milas region of southwest Turkey.
Arzu Arslan +2 more
exaly +4 more sources
Associated with the emplacement of the Lycian nappes, SW Turkey, Cretaceous limestones were thrusted over an ophiolitic melange in their front zone. Miocene flysch formed immediately in front of these nappes and were overthrusted by the Lycian nappes ...
Philippe Muchez +2 more
exaly +3 more sources

