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Evciler Plütonu’nun (KB Türkiye) Petrolojisi

Year 2018, Volume: 21 Issue: 2, 149 - 165, 30.06.2018

Şenel Özdamar

https://doi.org/10.17780/ksujes.392826
Cited By: 4

Abstract

Makale Şablonu



Oligo-Miyosen yaşlı
farklı boyutlarda ve jeokimyasal özelliklerde plütonlar Kuzey Batı Anadolu’da
yaygın yüzlek verirler. Bunlardan biriside Kazdağ metamorfiklerine sokulum
yapan KD-GB uzanımlı Evciler plütonudur. Plüton başlıca granodiyorit olmak
üzere kuvarslı monzonitik ve granitik kayaçlardan oluşmuş ve kuvars, plajiyoklas
(An26-41). K-feldspat (Or85-90), biotit (Mg#: 0.54), hornblend
(Mg#: 0.50-0.74) ana mineraller ile titanit. magnetit, ilmenit. apatit, zirkon
gibi tali minerallerin yanısıra ikincil minerallerden meydana gelmiştir.
Evciler plütonu çarpışma sonrası, I-tip  metalüminli ve yüksek potasyumlu kalk alkalen
özellikler sunar. İlksel mantoya göre normalize edilmiş iz element diyagramında
büyük iyon yarıçaplı elementler pozitif bir eğilim sergilerken, Nb, Pr, P ve Ti
ise negatif bir eğilim sergilemektedir. Kondrite göre normalize edilmiş nadir
toprak element diyagramında is Evciler örneklerinde bulunan
hafif nadir toprak elementler ağır nadir toprak elementlerine göre zenginlik
göstermektedir. Eu’un negatif ve Gd’nin pozitif anomalisi dikkat çekicidir. Tüm
bu veriler Evciler plütonunun çarpışma sonrası bir ortamda, zenginleşmiş
litosferik ergiyiklerinden oluşan ana mağmadan meydana geldiğini göstermektedir.




Keywords

Evciler jeokimya I-tip yüksek potasyumlu kalk alkalen

References

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  • Aghazadeh, M., Castro, A., Badrzadeh, Z., Vogt, K. 2011. Post-collisional polycyclic plutonism from the Zagros hinterland. The Shaivar-Dagh plutonic complex Alborz belt, Iran. Geological Magazine 148, 980-1008.
  • Akay, E. 2008. Geology and petrology of the Simav Magmatic Complex (NW Anatolia) and its comparison with the Oligo-Miocene granitoids in NW Anatolia: Implications on Tertiary tectonic evolution of the region. International Journal of Earth Sciences (doi 10.1007/s00531-008-0325-0).
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  • Altunkaynak, Ş., Dilek, Y., 2013. Eocene mafic volcanism in northern Anatolia: its causes and mantle sources in the absence of active subduction, International Geology Review, 55:13, 1641-1659,
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  • Karacık, Z., Yılmaz, Y., Pearce, J.A. and Ece, Ö.I. 2008. Petrochemistry of the south Marmara granitoids, northwest Anatolia, Turkey. International Journal of Earth Sciences, DOI 10.1007/s00531-007-0222-y.
  • Karaoğlu, Ö., Helvacı, C., 2014. Isotopic evidence for a transition from subduction to slabtear related volcanism in western Anatolia, Turkey. Lithos 192–195, 226–239.
  • Köksal, S., Toksoy-Köksal, F., Göncüoğlu, M.C., Möller, A., Gerdes, A., Frei, D. 2013. Crustal source of the Late Cretaceous Satansarı monzonite stock (central Anatolia–Turkey) and its significance for the Alpine geodynamic evolution. Journal of Geodynamics 65, 82-93.
  • Köprübasi, N., Aldanmaz, E. 2004. Geochemical constraints on the petrogenesis of Cenozoic I-type granitoids in Northwest Anatolia, Turkey: Evidence for magma generation by lithospheric delamination in a post-collisional setting: International Geology Review, 46: 705–729.
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Evciler Plütonu’nun (KB Türkiye) Petrolojisi

Year 2018, Volume: 21 Issue: 2, 149 - 165, 30.06.2018

Şenel Özdamar

https://doi.org/10.17780/ksujes.392826
Cited By: 4

Abstract



Oligo-Miyosen yaşlı
farklı boyutlarda ve jeokimyasal özelliklerde plütonlar Kuzey Batı Anadolu’da
yaygın yüzlek verirler. Bunlardan biriside Kazdağ metamorfiklerine sokulum
yapan KD-GB uzanımlı Evciler plütonudur. Plüton başlıca granodiyorit olmak
üzere kuvarslı monzonitik ve granitik kayaçlardan oluşmuş ve kuvars, plajiyoklas
(An26-41). K-feldspat (Or85-90), biotit (Mg#:0.54), hornblend
(Mg#:0.50-0.74) ana mineraller ile titanit. magnetit, ilmenit. apatit, zirkon
gibi tali minerallerin yanısıra ikincil minerallerden meydana gelmiştir.
Evciler plütonu çarpışma sonrası, I-tip  metalüminli ve yüksek potasyumlu kalk alkalen
özellikler sunar. İlksel mantoya göre normalize edilmiş iz element diyagramında
büyük iyon yarıçaplı elementler pozitif bir eğilim sergilerken, Nb, Pr, P ve Ti
ise negatif bir eğilim sergilemektedir. Kondrite göre normalize edilmiş nadir
toprak element diyagramında is Evciler örneklerinde
bulunan hafif nadir toprak elementler ağır nadir toprak elementlerine göre
zenginlik göstermektedir. Eu’un negatif ve Gd’nin pozitif anomalisi dikkat
çekicidir. Tüm bu veriler Evciler plütonunun çarpışma sonrası bir ortamda,
zenginleşmiş litosferik ergiyiklerinden oluşan ana mağmadan meydana geldiğini
göstermektedir.



Keywords

Evciler jeokimya I-tip yüksek potasyumlu kalk alkalen

References

  • Ackerman, L., Krňanská, M., Siebel, W., Strnad, L. 2010. Geochemistry of the Drahotín and Mutěnín intrusions, West Bohemian shear zone, Bohemian massif: contrasting evolution of mantle-derived melts. Mineralogy and Petrology 99, 185-199.
  • Aghazadeh, M., Castro, A., Badrzadeh, Z., Vogt, K. 2011. Post-collisional polycyclic plutonism from the Zagros hinterland. The Shaivar-Dagh plutonic complex Alborz belt, Iran. Geological Magazine 148, 980-1008.
  • Akay, E. 2008. Geology and petrology of the Simav Magmatic Complex (NW Anatolia) and its comparison with the Oligo-Miocene granitoids in NW Anatolia: Implications on Tertiary tectonic evolution of the region. International Journal of Earth Sciences (doi 10.1007/s00531-008-0325-0).
  • Altunkaynak, Ş., Yilmaz Y. 1998. The mount Kozak magmatic complex, Western Anatolia: Journal of Volcanology and Geothermal Research, 85, 211–131.
  • Altunkaynak, Ş., Dilek, Y., Genç, Ş.C., Sunal, G., Gertisser, R., Furnes, H., Foland, K.A., Yang, Y., 2012. Spatial, temporal and geochemical evolution of Oligo–Miocene granitoid magmatism in western Anatolia, Turkey. Gondwana Research 21, 961–986.
  • Altunkaynak, Ş., Dilek, Y., 2013. Eocene mafic volcanism in northern Anatolia: its causes and mantle sources in the absence of active subduction, International Geology Review, 55:13, 1641-1659,
  • Aydoğan, M.S. 2006. Baklan Graniti (Murat Dağı, Banaz/Uşak) civarındaki baz metal cevherleşmesinin mineral parajenezi, metal zonlanması ve kökenlerinin izotop jeokimyası ile saptanması. Süleyman Demirel Üniversitesi, Fen Bilimleri Enstitüsü, Doktora Tezi, 230 s.
  • Aydoğan, M.S., Çoban, H., Bozcu, M., Akıncı, Ö. 2008. Geochemical and mantle-like isotopic (Nd, Sr) composition of the Baklan Granite from the Muratdağı Region (Banaz, Uşak), western Turkey: Implications for input of juvenile magmas in the source domains of western Anatolia Eocene-Miocene granites. Journal of Asian Earth Sciences, 33: 155–176.
  • Bacon, C.R., Druitt, T.H. 1988. Compositional Evolution of the Zoned Calc-Alkaline Magma Chamber of Mount Mazama, Crater Lake, Oregon. Contribution to Mineralogy and Petrology 98, 224-256.
  • Barbarin, B., Didier, J., 1992. Genesis and evolution of mafic microgranular enclaves through various types of interaction between coexisting felsic and mafic magmas. Trans. R. Soc. Edinburgh: Earth Sci. 83, 145–153.
  • Boynton, W.V., 1984. Geochemistry of the rare-earth elements: meteorite studies. In: Henderson, P. (Ed.), Rare Earth Element Geochemistry. Elsevier, Amsterdam, 63–114.
  • Bozkurt, E. 2004. Granitoid rocks of the southern Menderes Masif (southwestern Turkey): Field evidence for Tertiary magmatism in an extensional shear zone: International Journal of Earth Sciences (Geologische Rundschau), 93: 52–71.
  • Bullen, T.D., Clynne, M.A., 1990. Trace Element and Isotopic Constraints on Magmatic Evolution at Lassen Volcanic Center. Journal of Geophysic Research 95, 19671-19691.
  • Chappell, B.W., White, A.J.R., Wyborn, D., 1987. The importance of residual source material restite in granite petrogenesis. J. Petrol. 28, 1111–1138.
  • Chen, W., Arculus, R.J. 1995. Geochemical and isotopic characteristics of lower crustal xenoliths, San Francisco Volcanic Field, Arizona, U.S.A. Lithos 110, 99-119.
  • Condie, K.C. 1993. Chemical composition and evolution of the upper continental crust: contrasting results from surface samples and shales. Chemical Geology 104, 1-37.
  • Deer, W.A., Howie R.A., Zussman, J.,1992). An Introduction to the Rock Forming Minerals (2nd edn). Longman Group Ltd, London.
  • Delaloye, M., Bingöl, E., 2000. Granitoids from Western and Northwestern Anatolia: geochemistry and modelling of geodynamic evolution. Inernational Geology Review, 42, 241-268.
  • Fitton, J.G., James, D., Leeman, W.P. 1991. Basic magmatism associated with late Cenozoic extension in the western United States: Compositional variations in space and time. Journal of Geophysical Research 96, 13693-13711.
  • Gagnevin, D., Daly, J.S., Poli, G. 2004. Petrographic, geochemical and isotopic constraints on magma dynamics and mixing in the Miocene Monte Capanne monzogranite (Elba Island, Italy). Lithos 78, 1-2, 157-195.
  • Genç, Ş.C., 1998. Evolution of the Bayramiç magmatic complexs, northwestern Anatolia Jour. Volcanol. Geotherm. Res., 85, 233-250.
  • Grove, T.L., Donnelly-Nolan, J.M. 1986. The Evolution of Young Silicic Lavas at Medicine Lake Volcano, California: Implications for the Origin of Compositional Gaps in Calc-Alkaline Series Lavas. Contributions to Mineralogy and Petrology 92, 281-302.
  • Güleç¸ N. 1991. Crust-mantle interaction in western Turkey: implications from Sr and Nd isotope geochemistry of Tertiary and Quaternary volcanics. Geol Mag 23:417-435.
  • Harris, N.B.W., Kelley, S., Okay, A., 1994. Post-collision magmatism and tectonics in northwest Anatolia. Contrib. Mineral. Petrol. 117, 241-252.
  • Hofmann, A.W. 1988. Chemical differentiation of the Earth: the relationship between mantle, continental crust, and oceanic crust. Earth and Planetary Science Letters 90, 297-314.
  • Işık, V., Tekeli, O., Seyitoglu, G., 2004. The 40Ar/39Ar age of extensional ductile deformation and granitoid intrusions in the northern Menderes core complex: Implications for the initiation of extensional tectonics in western Turkey. J. Asian Earth Sci. 23: 555-566.
  • Jahn, B.M., Zhang, Z.Q. 1984. Archean granulite gneisses from eastern Hebei Province, China: rare earth geochemistry and tectonic implications. Contribution to Mineralogy and Petrology 85, 224-243.
  • Karacık, Z., Yilmaz, Y. 1998. Geology of the ignimbrites and the associated volcano-plutonic complex of the Ezine area, northwestern Anatolia: Journal of Volcanology and Geothermal Research, 85: 251–264.
  • Karacık, Z., Yılmaz, Y., Pearce, J.A. and Ece, Ö.I. 2008. Petrochemistry of the south Marmara granitoids, northwest Anatolia, Turkey. International Journal of Earth Sciences, DOI 10.1007/s00531-007-0222-y.
  • Karaoğlu, Ö., Helvacı, C., 2014. Isotopic evidence for a transition from subduction to slabtear related volcanism in western Anatolia, Turkey. Lithos 192–195, 226–239.
  • Köksal, S., Toksoy-Köksal, F., Göncüoğlu, M.C., Möller, A., Gerdes, A., Frei, D. 2013. Crustal source of the Late Cretaceous Satansarı monzonite stock (central Anatolia–Turkey) and its significance for the Alpine geodynamic evolution. Journal of Geodynamics 65, 82-93.
  • Köprübasi, N., Aldanmaz, E. 2004. Geochemical constraints on the petrogenesis of Cenozoic I-type granitoids in Northwest Anatolia, Turkey: Evidence for magma generation by lithospheric delamination in a post-collisional setting: International Geology Review, 46: 705–729.
  • Lan, T.G., Fan, H.R., Santosh, M., Hu, F.F., Yang, K.F., Yang, Y.H., Yang, Y.H., Liu, Y.S. 2013. Crust–mantle interaction beneath the Luxi Block, eastern North China Craton: evidence from coexisting mantle- and crust-derived enclaves in a quartz monzonite pluton. Lithos 177, 1-6.
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There are 61 citations in total.

Details

Primary Language Turkish
Subjects Engineering
Journal Section Geological Engineering
Authors

Şenel Özdamar 0000-0002-4706-8585

Publication Date June 30, 2018
Submission Date February 12, 2018
Published in Issue Year 2018Volume: 21 Issue: 2

Cite

APA Özdamar, Ş. (2018). Evciler Plütonu’nun (KB Türkiye) Petrolojisi. Kahramanmaraş Sütçü İmam Üniversitesi Mühendislik Bilimleri Dergisi, 21(2), 149-165. https://doi.org/10.17780/ksujes.392826

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