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MANTO PERİDOTİTLERİNDE KISMİ ERGİME VE METAZOMATİZMA ETKİSİ: KIZILDAĞ OFİYOLİTİ ÖRNEĞİ (HATAY, TÜRKİYE)

Yıl 2024, Cilt: 27 Sayı: 3, 908 - 928, 03.09.2024

Mustafa Eren Rizeli , A. Feyzi Bingol , Abdullah Sar , Kuo-lung Wang

https://doi.org/10.17780/ksujes.1437482

Öz

Kızıldağ Ofiyoliti GD Anadolu Ofiyolit Kuşağı’nda yer alır ve tabandan tavana doğru manto peridotitleri, mafik/ultramafik kümülatlar, izotropik gabrolar, levha-dayk karmaşığı, plajiyogranitler ve volkanik kayaçlardan oluşmaktadır. Manto peridotitlerinde yapılan detaylı arazi çalışmaları ve petrografik gözlemler neticesinde seçilen örneklerin tüm kayaç ana oksit ve iz ve NTE içerikleri belirlenmiştir. Genellikle harzburjit ve az miktarda dünitten oluşan kayaçlar taneli ve elek dokular sergilemektedir. İlksel üst mantoya bileşimine kıyasla farklı derecelerde tüketilmiş olan kayaçlar; düşük Al2O3, CaO, TiO2 ve yüksek MgO içeriklerine sahiptir. Bazı örneklerde yüksek çekim alanlı elementler ve büyük iyon çaplı elementlerin bir kısmında zenginleşmeler görülmektedir. Arazide peridotitleri kesen ortopiroksenit kanallarının varlığı; petrografik olarak ikincil klinopiroksen oluşukları, kurtçuk şekilli (worm-like) piroksen-spinel simplektitler, olivinlerin spineller içinde kapanımı; jeokimyasal olarak bazı örneklerdeki iz element zenginleşmeleri (Cs, Rb, Ti, Sr, Pb, Ce, Zr/Hf ve Th/La) yiten levhadan türeyen sulu akışkanların ve ergiyiklerin metazomatizmasının bir sonucudur. Sonuç olarak Kızıldağ manto peridotitleri, %20’den fazla oranda tüketilmiş ve yitim zonu ortamını karakterize eden metazomatizma kanıtları gösteren yay önü peridotitleridir. .

Anahtar Kelimeler

jeokimya kısmi ergime Kızıldağ Ofiyoliti metazomatizma

Destekleyen Kurum

TÜBİTAK

Proje Numarası

117Y303

Kaynakça

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PARTIAL MELTING AND METASOMATISM EFFECTS IN MANTLE PERIDOTITES: THE CASE OF KIZILDAĞ OPHIOLITE (HATAY, TURKEY)

Yıl 2024, Cilt: 27 Sayı: 3, 908 - 928, 03.09.2024

Mustafa Eren Rizeli , A. Feyzi Bingol , Abdullah Sar , Kuo-lung Wang

https://doi.org/10.17780/ksujes.1437482

Öz

The Kızıldağ ophiolite is located in the SE Anatolian Ophiolite Belt and composed, from bottom to top, of mantle peridotites, mafic-ultramafic cumulates, isotropic gabbros, sheeted-dyke complex, plagiogranites and volcanic rocks. Based on detailed field studies and petrographic observations in mantle peridotites, selected samples' major oxide, trace, and REE contents were determined for the whole rock. The investigated rocks, generally composed of harzburgite and a small amount of dunite, display granoblastic and mesh textures. Rocks that have been depleted to different degrees compared to the composition of the primordial upper mantle have low Al2O3, CaO, TiO2, and high MgO contents. Enrichments in high-field strength elements and large ion lithophile elements are observed in some samples. Presence of orthopyroxenite channels cutting peridotites in the field; petrographically, secondary clinopyroxene formations, worm-like pyroxene-spinel symplectites, olivine inclusions within spinels; geochemically, trace element enrichments (Cs, Rb, Ti, Sr, Pb, Ce, Zr/Hf and Th/La) in some samples are a result of the metasomatism of aqueous fluids and melts derived from the subducted slab. As a result, Kızıldağ mantle peridotites are fore-arc peridotites that have been depleted by more than 20% and show evidence of metasomatism that characterizes the subduction zone environment.

Anahtar Kelimeler

Geochemistry partial melting Kızıldağ ophiolite mantle peridotite metasomatism

Proje Numarası

117Y303

Kaynakça

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  • Saka, S., Uysal, I., Kapsiotis, A., Bağcı, U., Ersoy, E. Y., Su, B.-X., Seitz, H.-M., Hegner, E. (2019). Petrological characteristics and geochemical compositions of the Neotethyan Mersin ophiolite (southern Turkey): Processes of melt depletion, refertilization, chromitite formation and oceanic crust generation. Journal of Asian Earth Sciences, 176, 281–299. https://doi.org/10.1016/J.JSEAES.2019.01.003
  • Saka, S., Uysal, I., Akmaz, R. M., Kaliwoda, M., Hochleitner, R. (2014). The effects of partial melting, melt-mantle interaction and fractionation on ophiolite generation: Constraints from the late Cretaceous Pozanti-Karsanti ophiolite, southern Turkey. Lithos, 202–203, 300–316. https://doi.org/10.1016/j.lithos.2014.05.027
  • Selçuk, H. (1981). Étude géologique de la partie méridionale du Hatay (Turquie). Thèse de doctorat, Université de Genève, Switzerland
  • Seyler M., Lorand J.-P., Dick H.J.B. Drouin M. (2007). Pervasive melt percolation reactions in ultra-depleted refractory harzburgites at the Mid-Atlantic Ridge, 15° 20′N: ODP Hole1274A. Contrib. Mineral. Petrol., 153: 303-319.
  • Shirey, S.B. and Walker, R.J. (1995). Carius tube digestion for low-blank rhenium-osmium analyses, . Anal. Chim. Acta, cilt 67, ss. 2136-2141
  • Snow, J. E., and Dick, H. J. B. (1995). Pervasive magnesium loss by marine weathering of peridotite. Geochimica et Cosmochimica Acta, 59(20), 4219–4235. https://doi.org/10.1016/0016-7037(95)00239-V
  • Stern, R.J., Reagan, M., Ishizuka, O., Ohara, Y., Whattam, S. (2012). To understand subduction initiation, study forearc crust: to understand forearc crust, study ophiolites. Lithosphere 4, 469–483
  • Suhr, G., Kelemen, P., and Paulick, H. (2008). Microstructures in Hole 1274A peridotites, ODP Leg 209, Mid-Atlantic Ridge: Tracking the fate ofmelts percolating in peridotite as the lithosphere is intercepted. Geochem. Geophys. Geosyst., 9 (Q03012), 1–23. https://doi.org/10.1029/2007GC001726
  • Takazawa, E., Frey, F. A., Shimizu, N., Obata, M. (2000). Whole rock compositional variations in an upper mantle peridotite (Horoman, Hokkaido, Japan): Are they consistent with a partial melting process? Geochimica et Cosmochimica Acta, 64(4), 695–716. https://doi.org/10.1016/S0016-7037(99)00346-4
  • Tekeli, O., and Erendil, M., 1986. Geology and Petrology of the Kızıldağ Ophiolite (Hatay). Maden Tetk. ve Aram. Derg. 107, 21–37.
  • Tekeli, O., Aksay, A., Urgun, B. M., Işık, A. (1983). Geology of the Aladağ Mountains. In Proceedings of International Symposium on the Geology of the Taurus Belt (eds O. Tekeli & M. C. Göncüoğlu), pp. 143–58. MTA-Ankara, Turkey.
  • Tinkler, C., Wagner, J.J., Delaloye, M., Selçuk, H. (1981). Tectonic history of the Hatay ophiolites (south Turkey) and their interpretation with the Dead Sea rift. Tectonophysics, 72, 23–41. https://doi.org/10.1016/0040-1951(81)90085-8
  • Üner, T. (2020). Multi-stage evolution of forearc mantle peridotites of Kağızman Ophiolite (Ağrı-eastern Anatolia). Journal of African Earth Sciences, 161(April 2019), 103667. https://doi.org/10.1016/j.jafrearsci.2019.103667
  • Uysal, İ., Ersoy, E. Y., Karslı, O., Dilek, Y., Sadıklar, M. B., Ottley, C. J., Tiepolo, M., & Meisel, T. (2012). Coexistence of abyssal and ultra-depleted SSZ type mantle peridotites in a Neo-Tethyan Ophiolite in SW Turkey: Constraints from mineral composition, whole-rock geochemistry (major–trace–REE–PGE), and Re–Os isotope systematics. Lithos, 132–133, 50–69. https://doi.org/10.1016/J.LITHOS.2011.11.009
  • Uysal, İ., Kaliwoda, M., Karsli, O., Tarkian, M., Sadiklar, M.B., Ottley, C.J. (2007). Compositional variations as a result of partial melting and melteperidotite interaction in an upper mantle section from the Ortaca area, southwestern Turkey. Can. Mineral. 45, 1471-1493.
  • van Hinsbergen, D.J.J, Peters, K., Maffione, M., Spakman, W., Guilmette, C., Thieulot, C., Plümper, O., Gürer, D., Brouwer, F.M., Aldanmaz, E., Kaymakci, N. (2015) Dynamics of intraoceanic subduction initiation: 2. Suprasubduction zone ophiolite formation and metamorphic sole exhumation in context of absolute plate motions. Geochem Geophys Geosyst 16:1771–1785
  • Varfalvy, V., Hébert, R., Bedard, J. H., Laflèche, M. R. (1997). Petrology and geochemistry of pyroxenite dykes in upper mantle peridotites of the North Arm Mountain massif, Bay of Islands Ophiolite, Newfoundland: Implications for the genesis of boninitic and related magmas. Canadian Mineralogist, 35(2), 543–570. https://doi.org/10.1016/0009-2541(95)00140-9
  • Vernon R.H. (2004). A practical guide to rock microstructure. Cambridge Univ. Press, 606 pp.
  • Völkening, J., Walczyk, T. and Heumann, K.G. (1991). Osmium isotope ratio determinations by negative thermal ionization mass spectrometry, Int. J. Mass Spectrom. Ion Process. cilt 105, ss. 147-159
  • Workman, R. K., and Hart, S. R. (2005). Major and trace element composition of the depleted MORB mantle (DMM). Earth and Planetary Science Letters, 231(1–2), 53–72. https://doi.org/10.1016/j.epsl.2004.12.005
  • Xiong, F., Yang, J., Robinson, P. T., Xu, X., Liu, Z., Zhou, W., Feng, G., Xu, J., Li, J., Niu, X. (2017). High-Al and high-Cr podiform chromitites from the western Yarlung-Zangbo suture zone, Tibet: Implications from mineralogy and geochemistry of chromian spinel, and platinum-group elements. Ore Geology Reviews, 80, 1020–1041. https://doi.org/10.1016/j.oregeorev.2016.09.009
  • Zhou, M.-F, Robinson, P.T., Malpas, J., Edwards, S.J., Qi, L. (2005): REE and PGE geochemical constraints on the formation of dunites in the Luobusa ophiolite, southern Tibet. J. Petrol. 46, 615–639.
  • Zhou, M. -F., Robinson, P. T., Malpas, J., Li, Z. (1996). Podiform chromitites in the Luobusa ophiolite (Southern Tibet): Implications for melt-rock interaction and chromite segregation in the upper mantle. Journal of Petrology, 37(1), 3–21. https://doi.org/10.1093/petrology/37.1.3
Toplam 92 adet kaynakça vardır.

Ayrıntılar

Birincil Dil Türkçe
Konular Mineraloji-Petrografi
Bölüm Jeoloji Mühendisliği
Yazarlar

Mustafa Eren Rizeli 0000-0003-3725-3063

A. Feyzi Bingol 0000-0002-1767-1076

Abdullah Sar 0000-0002-9752-7807

Kuo-lung Wang 0000-0002-6447-2168

Proje Numarası 117Y303
Yayımlanma Tarihi 3 Eylül 2024
Gönderilme Tarihi 15 Şubat 2024
Kabul Tarihi 14 Nisan 2024
Yayımlandığı Sayı Yıl 2024Cilt: 27 Sayı: 3

Kaynak Göster

APA Rizeli, M. E., Bingol, A. F., Sar, A., Wang, K.-l. (2024). MANTO PERİDOTİTLERİNDE KISMİ ERGİME VE METAZOMATİZMA ETKİSİ: KIZILDAĞ OFİYOLİTİ ÖRNEĞİ (HATAY, TÜRKİYE). Kahramanmaraş Sütçü İmam Üniversitesi Mühendislik Bilimleri Dergisi, 27(3), 908-928. https://doi.org/10.17780/ksujes.1437482
 Kapak Resmi İndir