Browsing Jeoloji Mühendisliği Bölümü by Publisher "Slovak Acad Sciences Geological Inst"
Now showing items 1-5 of 5
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Geochemistry And Origin Of Plagiogranites From The Eldivan Ophiolite, Cankiri (Central Anatolia, Turkey)
(Slovak Acad Sciences Geological Inst, 2014)The Eldivan Ophiolite, exposed around Ankara and Cankiri cities, is located at the central part of the Izmir-Ankara-Erzincan Suture Zone (IAESZ). It represents fragments of the Neotethyan Oceanic Lithosphere emplaced towards ... -
New Age Data From The Tectonostratigraphic Units Of The Istranca "Massif" In Nw Turkey: A Correlation With Se Bulgaria
(Slovak Acad Sciences Geological Inst, 2013)The Istranca Crystalline Complex in NW Anatolia and SE Bulgaria includes structural units that differ in lithostratigraphy, metamorphism, age and structural position. They are collectively named as the "Istranca nappes" ... -
Polyphase Tectonic Evolution of the Aksu Basin, Isparta Angle (Southern Turkey)
(Slovak Acad Sciences Geological Inst, 2015)The Aksu Basin, within the Isparta Angle, is located to the north of the intersection of the Aegean and Cyprus arcs and has been evolving since the Middle Miocene. Correlation of: (1) kinematic analysis of fault planes ... -
The Ankara Melange: An Indicator of Tethyan Evolution of Anatolia
(Slovak Acad Sciences Geological Inst, 2016)The Ankara Melange is a complex formed by imbricated slices of limestone block melanges (Karakaya and Hisarlikaya Formations), Neotethyan ophiolites (Eldivan, Ahlat and Edige ophiolites), post-ophiolitic cover units (Mart ... -
The Role Of Oroclinal Bending In The Structural Evolution Of The Central Anatolian Plateau: Evidence Of A Regional Changeover From Shortening To Extension
(Slovak Acad Sciences Geological Inst, 2011)The NW-SE striking extensional Inonu-Eskisehir Fault System is one of the most important active shear zones in Central Anatolia. This shear zone is comprised of semi-independent fault segments that constitute an integral ...
