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GEOLOGY OF THE KÜTAHYA-BOLKARDAĞ BELT

Yıl 2011, Cilt: 142 Sayı: 142, 223 - 277, 01.11.2011

Öz

Kütahya-Bolkardağ Belt is one of the subunits of the
Tauride-Anatolide Terrane extending from the Aegean Sea to the Hınzır
Mountains. It includes numerous tectonic slices, formed during the closure of
the İzmirAnkara Oceanic branch of the Neotethys. The tectonic slices are mainly
derived from three different tectonic settings: i- rocks representing the
oceanic lithosphere and subduction- accretion prism of the İzmirAnkara Ocean
(ophiolites and ophiolitic mélanges), ii- flysch-type deposits that were formed
in foreland-basins on the northern and passive edge of the Tauride-Anatolide
platform in front of the southward advancing nappes (olistostromes with
olistoliths, sedimentary mélanges), and iii- successions, in some cases with
HP/LT metamorphism, representing the slope margin and external platform of the
northern Tauride-Anatolide margin. Rock-units of the Kütahya-Bolkardağ Belt
surround the HT/LP Menderes Core Complex and are also observed as slices or
klippen in the massif, or as nappes to the south of it. The rocks of the İzmir-Ankara
oceanic lithosphere occur as huge allochthonous bodies/tectonic slices and
blocks within the mélange and olistostromes. The fossil data and geochemical
data obtained suggest the following: The earliest "oceanic" volcanism
commenced during middle Carnian, the generation of ocean island-type (OIB)
volcanics lasted from Bajocian to Abtian, where as the MORbasalts spread from
Aalenian to Turonian. Supra-subduction- and island-arc type basalts of Albian
to Cenomanian age indicate an intra-oceanic subduction within the İzmir-Ankara
Ocean. The mélanges are characterized by HP/LT metamorphism with a LP/LT
overprint. Middle Maestrichtian olistostomes with olistoliths formed in
foreland basins in front of the nappes include blocks of all kind of tectonic
settings mentioned above. The flysch rocks are in depositional contact with the
underlying platform and/or slope rocks of the Tauride-Anatolide passive margin.
The Tauride-Anatolide slope and external platform deposits are partly affected
by HP/LT metamorphism and occur as slices along the belt and as blocks within
the flysch-basins. In Afyon area the Late Permian transgresses onto the
Precambrian basement, whereas in Konya, more internal in regard to the
platform, the Devonian carbonate platform is drowned and covered by
back-arc-type sediments and volcanism of Carboniferous age. All along the belt,
early Late Permian unconformably covers a slightly metamorphosed and deformed
basement, attributed to a Variscan event within the Tauride-Anatolide platform.
The Lower Triassic sequences unconformably covering the older units and
starting with volcanogenic continental clastics, pass into the marine
carbonates by Anisian. In the allochtonous belonging to the more internal
platform, the Ladinian-Lower Cretaceous sequences are represented with thick
platform carbonates. The first deep marine sediments take place in some slices
of these sequences which is interpreted as the initial rifting of the İzmir-Ankara
oceanic branch. While only the slope sediments accompanying with transitional
ocean crust volcanics are observed in the allochtonous derived from the
northernmost part of the Taurid-Anatolid platform, the Ladinian-Lower
Cretaceous sequences are represented by thick platform carbonates in the
allochtonous of the inner platform. The transition from platform to slopetype
deposits is in Malm in the allochtonous of the external platform, but Abtian in
more internal parts. This indicates a stepwise deepening of the
platform-margin. The presence of HP/LT metamorphic platform-margin sediments is
indicative for a deep subduction of the attenuated continental-crust of the
Tauride-Anatolide margin. The initial compression-slicing and nappe-emplacement
must have realized prior to Middle Paleocene. Middle Paleocene-Middle Eocene in
the Kütahya-Bolkardağ Belt is characterized by shallow-marine or continental
molasse-type deposition in the remnant basins on the platform.

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Yıl 2011, Cilt: 142 Sayı: 142, 223 - 277, 01.11.2011

Öz


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  • Önen, P. and Hall, R., 1993. Ophiolites and related metamorphic rocks from the Kütahya region, north-west Turkey. Geological Journal, 28, 399- 412.
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  • , Göncüoðlu, M.C., Turhan, N., Uysal, Þ. and Þentürk, K., 1987. Late Palaezoic evolution of the Kütahya-Bolkardað Belt: Melih Tokay Geology Symposium, Ankara, Abstracts, 23- 24.
  • , and , 1989. Kütahya-Çifteler-Bayat- Ýhsaniye Yöresinin Temel Jeolojisi: Maden Tetkik ve Arama Genel Müdürlüðü Report no: 8974(8188), 142 s, Ankara (unpublished).
  • , , , Þentürk, K., Uysal, Þ. and Iþýk, A., 1990a. Konya-Kadýnhaný-Ilgýn Dolayýnýn Temel Jeolojisi: Maden Tetkik ve Arama Genel Mü- dürlüðü Report no: 9535, 132 p., Ankara (unpublished).
  • , , , Uysal, Þ. and Þentürk, K., 1990b. Late Palaezoic evolution of the KütahyaBolkardaðý Belt. Middle East Technical University Journal of Pure and Applied Sciences, 21/1-3, 211-220.
  • , Turhan, N. and Göncüoðlu, M.C., 1992. Field Guide to Kütahya Region. A Geotraverse Across Suture Zones In NW Anatolia, 9-11, Maden Tetkik ve Arama Genel Müdürlüðü Publication, Ankara.
  • Özer, S. and Ýrtem, O., 1982. Bornova Güneyi (Ýzmir) Üst Kretase kireçtaþlarýnýn stratigrafi ve fasiyes incelemesi: Türkiye Jeoloji Kurultayý, Ankara, Bildiri Özetleri, Özgül, N., 1976. Toroslarýn bazý temel jeoloji özellikleri. Geological Society Turkey Bulletin, 9, 65- 78.
  • and Kozlu, H., 2002. Kozan-Feke-Mansurlu arasýndaki bölgenin stratigrafisi ve tektonigine ait yeni veriler. Turkish Association Petroleum Geologists Bulletin, 14, 1-36.
  • Özgül, L. and Göncüoðlu, M.C., 1997. A HP/LT NeoTethyan sliver in the Northern Central Taurides, Turkey: Koçyaka Metaophiolitic Complex; remnant of a subducted passive continental margin: 20th Anniversy of Geological Education in Çukurova Universitesi, 30 April-3 May 1997, Adana, Abstracts, 3-4.
  • and 1998. Geology and petrology of HP/LT metamorphic rock units in Koçyaka Metamorphic Complex, Altýnekin Area, Konya: a HP/LT Neotethyan sliver in the northern Central Taurides. 3. International Turkish Geology Symposium, 31 August-4 September, 1998, Ankara, Abstracts, 277.
  • and 1999. Kocyaka metamorfik k ompleksinin metamorfik evrimi: Batý Orta Anadoluda YB/DS metamorfizmalý bir tektonik birim. 52. Türkiye Jeoloji Kurultayý. Abstracts, 279-286.
  • Özsayýn, E. and Dirik, K., 2008. Quaternary activity of the Cihanbeyli and Yeniceoba fault zones: Ýnönü-Eskiþehir fault system, Central Anatolia. Turkish Journal Earth Science, 16, 471-492
  • Rimmelé, G.T., Parra, B., Goffé, R., Oberhänsli, L., Jolivet, and Candan, O., 2005. Exhumation paths of high-pressure-low-temperature metamorphic rocks from the Lycian Nappes and the Menderes Massif (SW Turkey): a multi-equilibrium approach. Journal of Petrology, 46, 641- 669.
  • Robertson, A.H.F. and Pickett, E.A., 2000. Palaeozoicearly Tertiary Tethyan evolution in the Karaburun Peninsula (western Turkey) and Chios Island (Greece). In: Buzkurt, E., Winchester, J.A., Piper, J.D. (Eds.), Tectonics and Magmatism in Turkey and the Surrounding Area: Geological Society, London Special Publication, 173, 25-42.
  • Robertson, A.H.F. and Ustaömer, T., 2009. The Palaeozoic-early Mesozoic development of the Konya Complex, south central Turkey: testing of alternative subduction/accretion versus intra-continental marginal basin settings. Tectonophysics 473, 113-148.
  • Rojay, B., Yalýnýz, M.K. and Altýner, D., 1995. Age and origin of some spilitic basalts from 'Ankara Mélange' and their tectonic implications to the evolution of northern branch of Neotethys, Central Anatolia. International Earth Sciences Congree Aegean Regions Abstracts, Ýzmir.
  • Rosselet, F. and Stampfli, G., 2002. The Karaburun Units, a remnant of the Paleotethys fore-arc basin, in 1st International Symposium of the Faculty of Mines (ITU) on Earth Sciences and Engineering, 2002, Istanbul, Turkey.
  • Sherlock, S., Kelley, S.P., Inger, S., Harris, N., and Okay, A.I., 1999. 40Ar-39Ar and Rb-Sr geochronology of high-pressure metamorphism and exhumation history of the Tavþanlý Zone, NW Turkey. Contribution to Mineralogy and Petrology 137, 46-58.
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  • Þenel, M., Akdeniz, N., Öztürk, E.M., Özdemir, T., Kadýnkýzýn, G., Metin, Y., Özal, H., Serdaroðlu, M., and Örçen, S., 1994. Fethiye (Muðla)- Kallkan (Antalya) ve kuzeyinin jeolojisi. Maden Tetkik ve Arama Genel Müdürlüðü Report no: 9761, Ankara (unpublished).
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  • , Yalýnýz, M. K., and Altýner-Özkan, S., 2006. Neotetis Volkanitlerinin Planktonik Fosil Faunasý (Radyolarya ve Planktonik Foraminifera) ile Yaþlandýrýlmasý, Bornova Filiþ Zonu, KB Anadolu. Final Report TUBITAK Project 103Y027, 229p.
  • and 2007. Discovery of the oldest (upper Ladinian to middle Carnian) radiolarian assemblages from the Bornova Flysch Zone in western Turkey: Implications for the evolution of the Neotethyan Ýzmir-Ankara Ocean. Ofioliti, 32, 131-150.
  • Tekin, U.K. and Göncüoðlu, M.C., 2009. Late Middle Jurassic (Late Bathonian-Early Callovian) radiolarian cherts from the Neotethyan Bornova Flysch Zone, Spil Mountains, Western Turkey. Stratigraphy and Geological Correlation, 17/ 3, 298-308.
  • Turhan, N., Gürsu, S., and Göncüoðlu, M.C., 2003. Afyon yöresinde Prekambriyen temel ve Üst Paleozoyik-Alt Mesozoyik örtüsünün Stratigrafisi ve Jeolojisi. Mersin Üniversitesi 10.Yýl Sempozyumu., Abstract, 26-27.
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  • Wilson, J.L., 1975. Carbonate facies in geologic history. Springer Verl., NewYork, 265s.
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  • , and Floyd, P.A., 1998. Geochemistry and geodynamic setting of basic volcanics from the northernmost part of the Ýzmir-Ankara branch of Neotethys, Central Sakarya Region,Turkey. 3. International Turkish Geology Symposium, 31 August-4 September, 1998, Ankara, Abstracts, 174.
  • Yeniyol, M., 1982. Yunak (Konya) magnezitlerinin olu- þum sorunlarý, deðerlendirilmeleri ve yöre kayaçlarýnýn petrojenezi. Ýstanbul Yerbilimleri, 3/ 1-2, 21-51.
Toplam 121 adet kaynakça vardır.

Ayrıntılar

Birincil Dil İngilizce
Konular Mühendislik
Bölüm Makaleler
Yazarlar

M. Cemal Göncüoğlu

Yayımlanma Tarihi 1 Kasım 2011
Yayımlandığı Sayı Yıl 2011 Cilt: 142 Sayı: 142

Kaynak Göster

APA Göncüoğlu, M. C. (2011). GEOLOGY OF THE KÜTAHYA-BOLKARDAĞ BELT. Bulletin of the Mineral Research and Exploration, 142(142), 223-277.
AMA Göncüoğlu MC. GEOLOGY OF THE KÜTAHYA-BOLKARDAĞ BELT. Bull.Min.Res.Exp. Kasım 2011;142(142):223-277.
Chicago Göncüoğlu, M. Cemal. “GEOLOGY OF THE KÜTAHYA-BOLKARDAĞ BELT”. Bulletin of the Mineral Research and Exploration 142, sy. 142 (Kasım 2011): 223-77.
EndNote Göncüoğlu MC (01 Kasım 2011) GEOLOGY OF THE KÜTAHYA-BOLKARDAĞ BELT. Bulletin of the Mineral Research and Exploration 142 142 223–277.
IEEE M. C. Göncüoğlu, “GEOLOGY OF THE KÜTAHYA-BOLKARDAĞ BELT”, Bull.Min.Res.Exp., c. 142, sy. 142, ss. 223–277, 2011.
ISNAD Göncüoğlu, M. Cemal. “GEOLOGY OF THE KÜTAHYA-BOLKARDAĞ BELT”. Bulletin of the Mineral Research and Exploration 142/142 (Kasım 2011), 223-277.
JAMA Göncüoğlu MC. GEOLOGY OF THE KÜTAHYA-BOLKARDAĞ BELT. Bull.Min.Res.Exp. 2011;142:223–277.
MLA Göncüoğlu, M. Cemal. “GEOLOGY OF THE KÜTAHYA-BOLKARDAĞ BELT”. Bulletin of the Mineral Research and Exploration, c. 142, sy. 142, 2011, ss. 223-77.
Vancouver Göncüoğlu MC. GEOLOGY OF THE KÜTAHYA-BOLKARDAĞ BELT. Bull.Min.Res.Exp. 2011;142(142):223-77.

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