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Multi-Stage P-T-t Evolution of Precambrian Aged Rocks in Anamur (Alanya Massif, Mersin) Region

Yıl 2018, Cilt: 61 Sayı: 1, 90 - 130, 01.01.2018
https://doi.org/10.25288/tjb.358187

Öz

The Anamur region in the eastern part of the Alanya Massif is defined by high temperature metamorphism. Metamorphic rocks (Sarıağaç unit), under the conditions of the upper amphibolite facies which are interrupted by basic and acidic meta-magmatics in the region, constitute the para-autochtonous basis. Kapıdağ nappe, has undergone metamorphism the Barrow-type medium-pressure metamorphism in the greenschist facies is overlain by the tectonic contact of the Sarıağaç unit with the ductile conditions. The Kapıdağ nappe, which forms a regular and thick sequence, begins with a probable infra- cambrian aged assemblage in the base consisting of dolomite, marble, muscovite-quartz schist and chlorite schist alternation. This assemblage is overlain by low-grade metamorphics of Tauride units consist of quartzite, meta-carbonate and schists derived from Hüdai, Çaltepe and Seydişehir formations in Cambro-Ordovician aged. All these metamorphic units are unconformably overlain by conglomerates belonging to Late Eocene-Oligocene Anamur Formation and then Hadim nappe thrusted over to all units 
The metamorphism (M1) conditions of the high grade schists of the Sarıağaç unit are 7.7±0.7 kbar and 670±20°C. This high-grade assemblage underwent retrogration 5.1±0.3 kbar and 480±40°C (M2) in conditions. The dating of this metamorphism is 75-73 Ma (Campanian) based on Ar/Ar white mica aging. The age of M1 metamorphism could not be directly determined. Zircon ages of 550.2±8.2 Ma, which is interpreted as the age of crystallization of the primary acidic magmatics and the meta-aplites intersecting the regional foliation which is product of M1 metamorphism suggest that this metamorphism affecting the basement is probably Precambrian aged.
This data also reveals that the primary metaclastic rocks of the basement-forming metamorphic rocks are Precambrian aged. Given the paleogeographic location of the Alanya massif and geochronological data, the M1 metamorphism may be associated with the integration process of Gondwana’s Late Neoproterozoic. This high-grade basement was overprinted by the M2 metamorphism developed from the greenschist facies in the Late Cretaceous, associated with the closure of the southern part of the Neotethys ocean.

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Anamur (Alanya Masifi, Mersin) Bölgesinde Yer Alan Prekambriyen Yaşlı Kayaçların Çok Evreli P-T-t Evrimi

Yıl 2018, Cilt: 61 Sayı: 1, 90 - 130, 01.01.2018
https://doi.org/10.25288/tjb.358187

Öz

Alanya Masifi’nin doğu kesimde yer alan Anamur bölgesi yüksek sıcaklık metamorfizması ile tanımlanmaktadır. Bölgede bazik ve asidik meta-magmatikler tarafından kesilen, üst amfibolit fasiyesi koşullarında başkalaşıma uğramış metakırıntılılar (Sarıağaç birimi) paraotokton konumlu temeli oluşturmaktadır. Barrov türü orta basınç metamorfizmasının yeşilşist fasiyesi koşullarında başkalaşıma uğramış Kapıdağ napı, Sarıağaç birimini sünümlü koşullarda gelişmiş tektonik bir dokanakla üzerlemektedir. Düzenli ve kalın bir istif oluşturan Kapıdağ napı tabanda dolomit, mermer, muskovit- kuvars şist ve klorit şist ardalanmasından oluşan, olasılı İnfrakambriyen yaşlı topluluk ile başlamaktadır. Bu birim üzerine, Toros birliklerinin Kambro-ordovisiyen yaşlı Hüdai, Çaltepe ve Seydişehir formasyonlarından türeme, kuvarsit, meta-karbonat ve şistlerden yapılı düşük dereceli metamorfikler gelmektedir. Tüm bu metamorfik birimler Geç Eosen-Oligosen yaşlı Anamur Formasyonu’na ait çakıltaşları ile uyumsuz olarak örtülmekte ve Hadim napı tarafından tektonik olarak üzerlenmektedir.
Sarıağaç birimini oluşturan yüksek dereceli şistlerin metamorfizma (M1) koşulları 7.7±0.7 kbar basınç ve 670 ± 20°C sıcaklık olarak belirlenmiştir. Bu yüksek dereceli topluluk 5.1 ± 0.3 kbar basınç ve 480 ± 40°C sıcaklık koşullarında (M2) retrograd metamorfizmaya uğramıştır. Üzerleyen M2 metamorfizmasının yaşı beyaz mikalardan elde edilen Ar / Ar yaş belirlemesine göre 75 - 73 My (Kampaniyen) olarak bulunmuştur. M1 metamorfizmasının yaşı doğrudan belirlenememiştir. Fakat M1 metamorfizması ürünü bölgesel foliyasyonu kesen meta-aplitlerden elde edilen ve ilksel asidik magmatiklerin kristalizasyon yaşı olarak yorumlanan 550.2 ± 8.2 My U/Pb zirkon yaşları söz konusu temeli etkileyen bu metamorfizmanın olasılıkla Prekambriyen yaşlı olduğunu göstermektedir. Bu veri ayrıca temeli oluşturan metakırıntılıların ilksel kayalarının Prekambriyen yaşlı olduğunu ortaya koymaktadır. Alanya Masifi’nin paleocoğrafik konumu ve jeokronolojik veriler göz önüne alındığında, M1 metamorfizması Gondwana’nın Geç Neoproterozoyik’teki bütünleşme süreci ile ilişkilendirilebilmektedir. Bu yüksek dereceli temel Neotetis okyanusunun güney kolunun kapanması ile ilişkili olarak Geç Kretase’de yeşilşist fasiyesi koşullarından gelişen M2 metamorfizması tarafından üzerlenmiştir.

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  • Newton, R.C. ve Haselton, H.T., 1981. Thermodynamics of the garnetplagioclaseAlrSiOr-quartz geobarometer. In R C Newton, A Navrotsky, and B.J Wood, Eds, Advances in physical geochemistry, sayı l, s 131-147 Springer Verlag, New York
  • Okay A.I.,1989. An exotic eclogite/blueschist slice in a Barrovianstyle metamorphic terrain, Alanya Nappes, Southern Turkey. Journal of Petrology, 30(1), 107–132
  • Okay, A.I., 1997. Jadeite-K-feldspar rocks and jadeitites from northwest Turkey. Mineralogical Magazine, 61, 835-843.
  • Okay, A.I., 2002. Jadeite–chloritoid–glaucophane– lawsonite schists from northwest Turkey: unusually high P/T ratios in continental crust. Journal of Metamorphic Geology, 20, 757–768.
  • Okay, A.I. ve Özgül, N., 1984. HP/LT metamorphism and structure of the Alanya Massif, Southern Turkey: an allochthonous composite tectonic sheet. In: Robertson AHF, Dixon TE (ed) The geological evolution of the Eastern Mediterranean. Geological Society London Special Publication, 14, 429–439.
  • Okay, A.I. ve Tüysüz, O., 1999. Tethyan sutures of northern Turkey. In: Durand B, Jolivet L, Horváth F, Séranne M (eds) The Mediterranean Basins: Tertiary extension within the Alpine orogen. Geological Society London Special Publication,156, 475–515.
  • Okay, A.I, Satır, M., Maluski, H., Siyako, M., Monie, P., Metzger, R. ve Akyuz, S., 1996. Paleo- and NeoTethyan events in northwest Turkey: geological and geochronological constraints. In: Yin A, Harrison M (eds) Tectonics of Asia. Cambridge University Press, Cambridge, 520s.
  • Okay, A.I, Satır, M. ve Siebel, W., 2006. Pre-alpide orogenic events in the Eastern Mediterranean region. European lithosphere dynamics. Geological Society London Memoirs 32, 389–405.
  • Okay, A., Tansel, I. ve Tüysüz, O., 2001. Obduction, subduction and collision as reflected in the Upper Cretaceous–Lover Eocene sedimentary record of western Turkey. Geological Magazine, 138 (2), 117– 142.
  • Özgül, N., 1976. Toroslar’ın bazı temel jeoloji özellikleri. Türkiye Jeoloji Kurumu Bülteni 19, 65–78.
  • Özgül, N., 1984. Stratigraphy and tectonic evolution of the Central Taurides. International symposium on the geology of the Taurus Belt. Tekeli O, Göncüoğlu M.C. (ed), Ankara-Turkey, 77–90.
  • Özgül, N., 1997. Bozkır-Hadim-Taşkent (Orta Toroslarʹın Kuzey Kesimi) Dolaylarında Yer Alan Tektono – Stratigrafik Birliklerin Stratigrafisi. Maden Tetkik Arama Enstitüsü Dergisi, 119, 117–174.
  • Özgül, N. ve Gedik, İ., 1973. Orta Toroslar- da Alt Paleozoyik yaşta Çaltepe Kireç- taşı ve Seydişehir Formasyonu’nun stratigrafisi ve konodont faunası hakkında yeni bilgiler. Türkiye Jeoloji Kurumu Bülteni, 16(2), 39-52.
  • Özgül, N. ve Kozlu, H., 1992. Kozan-Feke-Mansurlu arasının jeolojisi. T.P.A.O. Rep. No:3380, 127s.
  • Özgül, N. ve Kozlu, H., 2002. Kozan-Feke (Doğu Toroslar) Yöresinin Stratigrafisi ve Yapısal Konumu ile İlgili Bulgular. Türkiye Petrol Jeologları Derneği Bülteni, 14(1),1-36.
  • Özgül, N., Metin, S. ve Dean, W. T., 1972. Doğu Toroslarʹda Tufanbeyli ilçesi (Adana) dolayının Alt Paleozoyik stratigrafisi ve faunası; Maden Tetkik Arama Enstitüsü Dergisi, 79, 9-17.
  • Parlak, O., Rızaoglu, T., Bagcı, U., Karaoglan, F. ve Höck, V., 2009. Tectonic significance of the geochemistry and petrology of ophiolites in southeast Anatolia, Turkey. Tectonophysics 473, 173–187.
  • Patrick, B. E. ve Evans, B. W., 1989. Metamorphic evolution of the Seward Peninsula blueschist terrane. Journal of Petrology, 30, 531–555.
  • Perchuk, L.L., 2004. Progress in Metamorphic and Magmatic Petrology: A Memorial Volume in Honour of D.S. Korzhinskiy. Ed. L.L. Perchuk. Cambridge University Press, 520 p.
  • Pognante, U., 1985. Coronitic reactions and ductile shear zones in eclogitized ophiolite metagabbro, western Alps, north Italy. Chemical Geology, 50, 99-109.
  • Pourteau, A., Sudo, O., Candan, O., Lanari, P., Vidal, O. ve Oberhansli, R., 2013, Neotethys closure history of Anatolia: insights from Ar geochronology and P–T estimation in highpressure metasedimentary rocks. Journal of Metamorphic Geology. 31(6), 585-606.
  • Proyer, A., 2003. The preservation of high-pressure rocks during exhumation: metagranites and metapelites. Lithos 70, 183–194.
  • Rubie, D.C., 1986. The catalysis of mineral reactions by water and restrictions onthe presence of aqueous fluıd during metamorphism. Mineralogical Magazine, 50, 399-415.
  • Rolland, Y., Billo, S., Corsini, M., Sosson, M. ve Galoyan, G., 2009. Blueschists of the Amassia–Stepanavan Suture Zone (Armenia): linking Tethys subduction history from E-Turkey to W-Iran. International Journal of Earth Science 98, 533–550
  • Satır, M., Friedrichsen, H., 1986. The origin and evolution of the Menderes Massif, W Turkey: a rubidium/strontium and oxygen isotope study. Geologische Rundschau.75, 703–714.
  • Schmidt, M. W., 1992. Amphibole composition in tonalite as a function of pressure: an experimental calibration of the Al-in-hornblende barometer. Contribution Mineralogy and Petrography,110, 304-310.
  • Schmidt, A., Pourteau, A., Candan O. ve Oberhansli R., 2015. Lu–Hf geochronology on cm-sized garnets using microsampling: New constraints on garnet growth rates and duration of metamorphism during continental collision (Menderes Massif, Turkey). Earth and Planetary Science Letters, 432, 24-35.
  • Sisson, V. B., Ertan, I. E. ve ave Lallemant, H. G., 1997. High pressure (2000 MPa) kyanite- and glaucophane-bearing pelitic schist and eclogite from Cordillera de la Costa Belt,Venezuela. Journal of Petrology, 38, 65–83.
  • Snee, L.W., Sutter, J.F. ve Kelly, W.C., 1988. Thermochronology of economic mineral deposits—Dating the stages of mineralization at Panasqueira, Portugal, by high-precision 40Ar/39Ar age-spectrum techniques on muscovite: Economic Geology, 83, 335–354.
  • Spear, F.S., 1993. Metamorphic Phase Equilibria and Pressure-Temperature-Time Paths. Mineralogical Society of America, Washington, D.C., 799pp
  • Şenel, M., Gedik, I., Dalkılıç, N., Serdaroğlu, M., Bilgin. A.Z,. Uğuz, M.F., Bölükbaşı. A.S., Korucu, M. ve Özgül, N., 1996. Isparta büklümü doğusunda otokton ve allokton birimlerin stratigrafisi (Batı Toroslar). Maden Tetkik Arama Enstitüsü Dergisi, 118, 111 -160.
  • Şengor, A.M.C., Görür, N. S. ve Karoğlu, F., 1985. Strike-slip faulting and related basin formation in zones of tectonic escape: Turkey as a case study. In: Biddle KT, Christie-Blick N (eds), Strike-slip deformation, Basin formation and sedimentation.Society Economic Mineral Paleontology and Mineralogy Special Publication, 37, 227–264
  • Şengör, A.M.C. ve Yılmaz,Y. 1981. Tethyan evolution of Turkey: a plate tectonic approach. Tectonophysics, 75,181–241.
  • Şengör, A.M.C., Yılmaz, Y. ve Ketin, I., 1980 Remnants of a pre-Late Jurassic ocean in the northern Turkey: fragments of Permian-Triassic PaleoTethys. Geological Society American Bulletin, 91(1), 599–609.
  • Şengör, A.M.C., Yilmaz, Y. Ve Sungurlu, O., 1984. Tectonics of the Mediterranean Cimmerides: nature and evolution of the western termination of Palaeo-Tethys. The Geological Evolution of the Eastern Mediterranean. In: Dixon, J.E., Robertson, A.H.F.(Eds.)., Geological Society, London, Special Publications 17, 77–112.
  • Tsujimori T., 2010. Prograde and terrograde P-T paths of the late paleozoic glaucophane eclogite from the Renge metamorphic belt, Hida Mountains, Southwestern Japan. International Geology Rewiew, 44(9), 797-818.
  • Tsujimori, T. ve Ernst W.G., 2014. Lawsonite blueshist and lawsonite eclogites as proxies for paleosubduction zone processes: a review. Journal of Metamorphic Geology,32(5), 437-454.
  • Tsujimori, T. ve Liou, J.G., 2007. Significance of the Ca-Na pyroxene-lawsonite-chlorite assemblage in blueschist-facies metabasalts: An example from the Renge metamorphic rocks, southwest Japan. International Geology Review 49 (5), 416-430
  • Tuccillo, M.E., Essene, E.J. ve van der Pluijm, B.A., 1990. Growth and retrograde zoning in garnets from high-grade metapelites: implications for pressure-temperature paths. Geology, 18, 839843.
  • Turan, A., 2000. Korualan Bağbaşı (Hadim-Konya) arasındaki bölgenin yapısal özellikleri; Dokuz Eylül Üniversitesi Fen ve Mühendislik Dergisi, 2(3), 51-60.
  • Turan, A., Kurtman, F. ve Seymen, İ., 2007 Toroslarda Hadım bölgesinin paleotektonik dönem jeolojik evrimi. Selçuk Üniversitesi Mühendislik Mimarlık Fakültesi Dergisi, 23,1-2.
  • Ulu, Ü., 1989. Gazipaşa (Antalya ili) bölgesinin jeolojisi Doktota Tezi, İ.Ü. Fen Bilimleri Enst., 209 s (Yayınlanmamış).
  • Ustaömer, P.A., Ustaömer, T., Collins, A.S. ve Robertson, A.H.F., 2009. Cadomian (Ediacaran–Cambrian) arc magmatism in the Bitlis Massif, SE Turkey: magmatism along the developing northern margin of Gondwana. Tectonophysics 473, 99–112.
  • Yalçın, N., 1980. Amanosların Litolojik Karakterleri ve Güneydoğu Anadolu’nun Tektonik Evrimindeki Anlamı. Türkiye Jeoloji Kurumu, 23,21-30
  • Yılmaz, Y., 1993. New evidence and model on the evolution of the southeast Anatolian orogen. Bulletin Geological Society of America, 105, 252–271.
Toplam 123 adet kaynakça vardır.

Ayrıntılar

Konular Yer Bilimleri ve Jeoloji Mühendisliği (Diğer)
Bölüm Makaleler - Articles
Yazarlar

Mete Çetinkaplan Bu kişi benim

Yayımlanma Tarihi 1 Ocak 2018
Gönderilme Tarihi 4 Eylül 2017
Kabul Tarihi 15 Aralık 2017
Yayımlandığı Sayı Yıl 2018 Cilt: 61 Sayı: 1

Kaynak Göster

APA Çetinkaplan, M. (2018). Anamur (Alanya Masifi, Mersin) Bölgesinde Yer Alan Prekambriyen Yaşlı Kayaçların Çok Evreli P-T-t Evrimi. Türkiye Jeoloji Bülteni, 61(1), 90-130. https://doi.org/10.25288/tjb.358187
AMA Çetinkaplan M. Anamur (Alanya Masifi, Mersin) Bölgesinde Yer Alan Prekambriyen Yaşlı Kayaçların Çok Evreli P-T-t Evrimi. Türkiye Jeol. Bült. Ocak 2018;61(1):90-130. doi:10.25288/tjb.358187
Chicago Çetinkaplan, Mete. “Anamur (Alanya Masifi, Mersin) Bölgesinde Yer Alan Prekambriyen Yaşlı Kayaçların Çok Evreli P-T-T Evrimi”. Türkiye Jeoloji Bülteni 61, sy. 1 (Ocak 2018): 90-130. https://doi.org/10.25288/tjb.358187.
EndNote Çetinkaplan M (01 Ocak 2018) Anamur (Alanya Masifi, Mersin) Bölgesinde Yer Alan Prekambriyen Yaşlı Kayaçların Çok Evreli P-T-t Evrimi. Türkiye Jeoloji Bülteni 61 1 90–130.
IEEE M. Çetinkaplan, “Anamur (Alanya Masifi, Mersin) Bölgesinde Yer Alan Prekambriyen Yaşlı Kayaçların Çok Evreli P-T-t Evrimi”, Türkiye Jeol. Bült., c. 61, sy. 1, ss. 90–130, 2018, doi: 10.25288/tjb.358187.
ISNAD Çetinkaplan, Mete. “Anamur (Alanya Masifi, Mersin) Bölgesinde Yer Alan Prekambriyen Yaşlı Kayaçların Çok Evreli P-T-T Evrimi”. Türkiye Jeoloji Bülteni 61/1 (Ocak 2018), 90-130. https://doi.org/10.25288/tjb.358187.
JAMA Çetinkaplan M. Anamur (Alanya Masifi, Mersin) Bölgesinde Yer Alan Prekambriyen Yaşlı Kayaçların Çok Evreli P-T-t Evrimi. Türkiye Jeol. Bült. 2018;61:90–130.
MLA Çetinkaplan, Mete. “Anamur (Alanya Masifi, Mersin) Bölgesinde Yer Alan Prekambriyen Yaşlı Kayaçların Çok Evreli P-T-T Evrimi”. Türkiye Jeoloji Bülteni, c. 61, sy. 1, 2018, ss. 90-130, doi:10.25288/tjb.358187.
Vancouver Çetinkaplan M. Anamur (Alanya Masifi, Mersin) Bölgesinde Yer Alan Prekambriyen Yaşlı Kayaçların Çok Evreli P-T-t Evrimi. Türkiye Jeol. Bült. 2018;61(1):90-130.

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