아나톨리아 반도의 지질구조: 대륙 충돌에 따른 구조적 성장 = Geologic Structure of the Anatolian Peninsula: Tectonic Growth of Collisional Continental Margins

다국어 초록 (Multilingual Abstract)

The Anatolia peninsula consists of several continental fragments that include the Pontide Block in north and the Anatolide-Touride Block in south as well as the Arabian Platform in southeast. These continental blocks were joined together into a single landmass in the late Tertiary. During most of the Phanerozoic these continental blocks were separated by paleo-oceans, such as Paleo-Tethys and Neo-Tethys. The Pontide Block in north show Laurasian affinities, and was only slightly affected by the Alpide orogeny; they preserve evidence for the Variscan and Cimmeride orogenies. The Pontic Block is composed of the Strandja, Istanbul and Sakarya zones that were amalgamated into a single terrane by the mid Cretaceous times. The Anatolide-Tauride Block in south shows Gondwana affinities but was separated from Gondwana in the Triassic and formed an extensive carbonate platform during the Mesozoic. The Anatolide-Tauride Block was intensely deformed and partly metamorphosed during the Alpide orogeny; this leads to the subdivision of the Anatolide-Tauride Block into several zones on the basis of the type and age of metamorphism and deformation. The Arabian Platform in southeast forms the northernmost extension of the Arabian Plate that shows a stratigraphy similar to the Anatolide-Tauride Block with a clastic-carbonate dominated Palaeozoic and a carbonate dominated Mesozoic succession. A new tectonic era started in Anatolia Peninsula in the Oligocene-Miocene after the final amalgamation of these continental blocks and plate. This neotectonic phase is characterized by extension, and strike-slip faulting, continental sedimentation, and widespread calcalkaline magmatism, which played a very important role in producing beautiful landscapes of the Anatolia Peninsula today.

참고문헌 (Reference)

1 이길재, "터키 지질 및 광물자원 현황" 한국광물학회 25 (25): 51-61, 2012

2 Okay, A.I, "Tethyan sutures of northern Turkey" 156 : 475-515, 1999

3 Whitney, D.L, "Tectonic controls on metamorphism, partial melting, and intrusion: Timing of regional metamorphism and magmatism of the Ni e Massif, Turkey" 376 : 37-60, 2003

4 Juras, S, "Technical report for the Kisladag gold mine, Turkey" the Eldorado Gold Corporation 120-, 2010

5 Göoncüuoglu, M.C, "Pre- Alpine and Alpine Terranes in Turkey: explanatory notes to the terrane map of Turkey" 37 : 515-536, 1997

6 Karao lu, Ö, "Petrogenesis and 40Ar/39Ar geochronology of the volcanic rocks of the U ak-Güre basin, western Türkiye" 119 : 193-210, 2011

7 Yilmaz, Y, "New evidence and model on the evolution of the southeast Anatolian orogen" 105 : 252-271, 1993

8 Whitney, D.L, "Metamorphic and Tectonic Evolution of the H kada k Block, Central Anatolian Crystalline Complex" 10 : 1-15, 2001

9 Monod, O, "Late Ordovician glaciation in southern Turkey" 15 : 249-257, 2003

10 Yalccin, N, "Geology of the Narince-Gerger area (Ad yaman province) and its petroleum possibilities" 41 : 57-82, 1976

11 Okay, A.I, "Geology of Turkey: A Synopsis" 21 : 19-42, 2008

12 Erler, A, "Geologic and tectonic setting of Yozgat batholith, northern central Anatolian crysttaline complex, Turkey" 38 : 714-726, 1996

13 Ak man, O, "Geochemical characteristics of granitoids along the western margin of the Central Anatolian Crystalline Complex and their tectonic implications" 28 : 371-382, 1993

14 Çelik, Ö.F, "Early-Middle Jurassic intraoceanic subduction in the zmir-Ankara-Erzincan Ocean, Northern Turkey" 509 : 120-134, 2011

15 Kaya, C, "Deep crustal structure of northwestern part of Turkey" 489 : 227-239, 2010

16 Huvaz, O, "Comparative petroleum systems analysis of the interior basins of Turkey: Implications for petroleum potential" 26 : 1656-1676, 2009