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Petrographic and geochemical analyses of Early Miocene volcanic units in the Bigadiç borate basin, western Anatolia-Turkey: evidences of magma mixing/mingling processes

Yıl 2010, Cilt: 31 Sayı: 2, 141 - 168, 01.03.2010

Öz

Kaynakça

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Erken Miyosen Bigadiç bor havzasındaki volkanik birimlerin petrografik ve jeokimyasal özellikleri: magma karışımının kanıtları, Batı Anadolu-Türkiye

Yıl 2010, Cilt: 31 Sayı: 2, 141 - 168, 01.03.2010

Öz

Batı Anadolu’daki Senozoyik yaşlı alkali ve kalkalkali karakterli volkanizmanın en iyi gözlendiği bölgelerden birisi kuzeydoğu doğrultulu Bigadiç bor havzasıdır. Bazalttan riyolite bileşim gösteren volkanik kayaçların oluşum yaşları 23-17.8 milyon yıl arasındadır. Bigadiç çevresinde, temel kayaçlar üzerindeki Erken Miyosen yaşlı istifler gölsel, flüvyal ve evaporitik tortullar ile bunları kesen kuzeydoğu doğrultulu volkanik çıkış merkezlerinden üretilen lav ve volkaniklastik kayaçlar ile temsil edilmektedir. İki farklı evrede gelişen bu volkanik birimler litolojik, petrografik ve bileşimsel özelliklerine göre, Kocaiskan volkanik birimi, Gölcük bazaltı, Sındırgı, Kayırlar ve Şahinkaya volkanik birimleri olmak üzere beş birim altında incelenmiştir. Gölcük bazaltı hariç, diğer tüm volkanik birimlerde yaygın olarak görülen yuvarlağımsı elipsoidal anklavların boyutları birkaç milimetreden birkaç santimetreye kadar değişmektedir. Kalkalkali bileşim sergileyen Kocaiskan, Sındırgı, Şahinkaya ve Kayırlar volkanik birimleri orta-yüksek, hafif alkali bileşimli Gölcük bazaltı ise yüksek K’ludur. Kalkalkali birimlerin nadir toprak element dağılım desenleri birbirlerine benzerlik göstermektedir. Bu birimler hafif nadir toprak elementlerince zenginleşme gösterirken, hafif alkali bileşimli Gölcük bazaltında ise daha az zenginleşme görülmektedir. Eu anomalisi Kocaiskan ve Sındırgı volkanik birimlerinde, Şahinkaya, Kayırlar ve Gölcük birimlerine göre daha belirgindir. Bigadiç ve çevresinde eş yaşlı alkali-kalkalkali birlikteliği ile karakterize bimodal volkanik kayaçların oluşumunda, magma karışım süreçleri etkili olup, kabuksal kökenli ve manto kökenli iki farklı magma kaynağı etkindir

Kaynakça

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  • Aldanmaz, E., Pearce, J.A., Thirlwall, M.F., and Mitchell, J.G., 2000. Petrogenetic evo- lution of late Cenozoic, post-collision volcanism in the western Anatolia, Tur- key. Journal of Volcanology and Geot- hermal Research, 102, 67-95.
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  • Altunkaynak, Ş., and Dilek, Y., 2006. Timing and nature of postcollisional volca- nism in western Anatolia and geody- namic implications. In: Y. Dilek and S. Pavlides (eds.), Postcollisional Tecto- nics and Magmatism in the Mediterra- nean Region and Asia: Geological Soci- ety of American Special Paper 409, pp. 321-351.
  • Altunkaynak, S., Rogers, N. W., and Kelley, S. P., 2010. Causes and effects of geoc- hemical variations in late Cenozoic vol- canism of the Foça volcanic centre, NW Anatolia, Turkey. International Geology Review, 52, 579-607.
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Toplam 169 adet kaynakça vardır.

Ayrıntılar

Birincil Dil Türkçe
Bölüm Makaleler
Yazarlar

Fuat Erkül Bu kişi benim

Sibel TATAR Erkül Bu kişi benim

Cahit Helvacı Bu kişi benim

Yayımlanma Tarihi 1 Mart 2010
Gönderilme Tarihi 24 Mart 2015
Yayımlandığı Sayı Yıl 2010 Cilt: 31 Sayı: 2

Kaynak Göster

EndNote Erkül F, Erkül ST, Helvacı C (01 Mart 2010) Erken Miyosen Bigadiç bor havzasındaki volkanik birimlerin petrografik ve jeokimyasal özellikleri: magma karışımının kanıtları, Batı Anadolu-Türkiye. Yerbilimleri 31 2 141–168.