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Mineral Chemistry, Geochemistry and Petrology of Oligocene-Miocene Calc-alkaline Volcanic Rocks in Büyükbostancı-Çiçekpınar (Balıkesir, NW Turkey)

Yıl 2022, Cilt: 65 Sayı: 2, 117 - 148, 15.04.2022

Ferhat Bozan Zafer Aslan

https://doi.org/10.25288/tjb.1018440

Öz

In this study, petrography, mineral chemistry, geochemistry, and petrology of Oligocene-Miocene volcanic rocks located in the Büyükbostancı-Çiçekpınar (Balıkesir, NW Turkey) region in the south of Balıkesir were investigated.

The studied volcanics rocks have the composition of andesite, basaltic andesite, trachyandesite, and
accompanying pyroclastics. Volcanic rocks show microlithic porphyry, porphyric, fluidal, glomeroporphyritic and spherulitic structures, and consist of plagioclase, clinopyroxene, amphibole, biotite, and Fe-Ti oxide as the major minerals. According to the results of mineral chemistry analysis of the investigated volcanic rocks, plagioclases are andesine (An33-47Ab49-61Or2-6) and labradorite (An60-62Ab34-38Or1-4), pyroxenes are augite and clinoenstatite (Wo43En75Fs36-Wo1En38Fs14), and biotite is Mg-bearing biotite. Geothermobarometry calculations from biotite yielded a temperature range of 798–843 °C and a pressure range of 0.67–1.93 kbar.

Geochemically, the volcanic rocks have high-K calc-alkaline features. Fractional crystallization and assimilation processes dominated by hornblende, clinopyroxene and biotite mineral differentiation affected the andesitic volcanic rocks. Trace element diagram for volcanic rocks normalized to normal-mid-ocean ridge basalts (N-MORB) show enrichment in large ion lithophile elements (LILE, Rb, U and Th) and depletion in high field strength elements (HFSE, Nb and Yb). In the rare earth element diagram normalized to chondrite, there is moderate enrichment of (La/Lu)N 8.29-15.65 and the curve generally has a concave shape. When the obtained data and regional geological data are evaluated together, the investigated volcanic rocks are post-collisional products with subduction traces and are derived from enriched lithospheric mantle.

Anahtar Kelimeler

Andesite Biga Peninsula Hallaçlar Volcanic Rocks geochemistry mineral chemistry

Proje Numarası

Proje No: 2018/049

Kaynakça

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Büyükbostancı-Çiçekpınar (Balıkesir, KB Türkiye) Yöresindeki Oligosen-Miyosen Yaşlı Kalk-alkalen Volkanik Kayaçların Mineral Kimyası, Jeokimyası ve Petrolojisi

Yıl 2022, Cilt: 65 Sayı: 2, 117 - 148, 15.04.2022

Ferhat Bozan Zafer Aslan

https://doi.org/10.25288/tjb.1018440

Öz

Bu çalışmada, Balıkesir ili güneyindeki Büyükbostancı-Çiçekpınar (Balıkesir, KB Türkiye) yöresinde bulunan, Oligosen-Miyosen yaşlı volkanik kayaçların petrografisi, mineral kimyası jeokimyası ve petrolojisi incelenmiştir.

Çalışılan volkanikler andezit, bazaltik andezit, trakiandezit ve piroklastik kayaçlardan oluşmaktadır. Mikrolitik porfirik, porfirik yer yer de fluidal, glomeroporfirik ve sferülitik dokuya sahip olan volkanik kayaçlar, plajiyoklaz, klinopiroksen, amfibol, biyotit ve Fe-Ti oksit ana minerallerden ibarettir. Çalışılan volkanik kayaçlara ait mineral kimyası analiz sonuçlarına göre, plajiyoklazlar andezin (An33-47Ab49-61Or2-6) ve labradorit (An60-62Ab34- 38Or1-4), piroksenler ojit ve klinoenstatit (Wo43En75Fs36-Wo1En38Fs14), biyotitler ise Mg’lu biyotit türündedir. Biyotit mineralinden jeotermobarometre hesaplamalarına göre, 798-843 °C sıcaklık ve 0,67-1,93 kbar basınç elde edilmiştir.

Jeokimyasal olarak, çalışılan volkanik kayaçlar yüksek K’lu kalk-alkalen özelliğe sahiptir. Andezitik volkanik kayaçlarda hornblend, klinopiroksen ve biyotit mineral ayrımlaşmasının hâkim olduğu fraksiyonel kristalleşme ve asimilasyon süreçleri etkili olmuştur. Volkanik kayaçların Normal-Okyanus Ortası Sırtı Bazaltları’na (N-OOSB) göre normalize iz element diyagramında, büyük iyon yarıçaplı litofil elementlerce (BİYE, Rb, U ve Th) zenginleşme izlenirken, yüksek çekim alanlı elementlerce (YÇAE, Nb ve Tb) ise fakirleşme görülmektedir. Kondrite göre normalize nadir toprak element dağılımları, (La/Lu)N 8,29-15,65 ile orta düzeyde zenginleşme göstermekte olup, genel olarak konkav bir dağılım sunmaktadır. Elde edilen veriler ile bölgesel jeolojik veriler birlikte değerlendirildiğinde, incelenen volkanik kayaçların yitim izi taşıyan çarpışma sonrası ürünler olduğu ve ayrıca zenginleşmiş litosferik mantodan türemiş olduğunu işaret etmektedir.

Anahtar Kelimeler

Andezit Biga Yarımadası Hallaçlar Volkanik Kayaçları jeokimya mineral kimyası

Destekleyen Kurum

Balıkesir Üniversitesi Bilimsel Araştırma Projeler Birimi

Proje Numarası

Proje No: 2018/049

Teşekkür

Bu çalışma, Balıkesir Üniversitesi Bilimsel Araştırma Projeler Birimi tarafından desteklenmiştir (Proje No: 2018/049).

Kaynakça

  • Akay, E. (2009). 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, 98, 1655-1675.
  • Aldanmaz, E., Pearce, J. A., Thirlwall, M. F. & Mitchell, J. G. (2000). Petrogenetic Evolution of late Cenozoic, Post-collision Volcanism in Western Anatolia, Turkey. Journal of Volcanology and Geothermal Research, 102, 67-95.
  • Altunkaynak, Ş. (2007). Collision-driven slab breakoff magmatism in northwestern Anatolia, Turkey. Journal of Geology, 115, 63-82.
  • Altunkaynak, Ş. & Dilek, Y. (2006). Timing and nature of postcollisional volcanism in western Anatolia and geodynamic implications. In: Dilek, Y. & Pavlides, S. (Eds.), Post collisional tectonics and magmatism in the Mediterranean region and Asia. Geological Society of America Special Paper, 409, 321–351.
  • Altunkaynak, Ş. & Genç, Ş. C. (2008). Petrogenesis and time-progressive evolution of the Cenozoic continental volcanism in the Biga Peninsula, NW Anatolia (Turkey). Lithos, 102, 316-340.
  • Altunkaynak, S., Dilek, Y., Genç, Ş. C., Sunal, G., Gertisser, R., Furnes, H., Foland, K. A. & Yang, J. (2012). Spatial, temporal and geochemical evolution of Oligo–Miocene granitoid magmatism in western Anatolia, Turkey. Gondwana Research, 21, 961-986.
  • Aslan, Z., Edrem, D., Temizel, İ. & Arslan, M. (2017). SHRIMP U–Pb zircon ages and whole-rock geochemistry for the Şapçı volcanic rocks, Biga Peninsula, Northwest Turkey: implications for pre-eruption crystallization conditions and source characteristics. International Geology Review, 59(14), 1764-1785.
  • Aslan, Z., Demir, H. & Altın, İ. (2020). U–Pb zircon geochronology and petrology of the early Miocene Göloba and Şaroluk plutons in the Biga Peninsula, NW Turkey: Implications for post-collisionalmagmatism and geodynamic evolution. Journal of African Earth Sciences, 172, Article 103998.
  • Aysal, N., Öngen, A. S., Yılmaz Şahin, S., Kasapçı, C., Hanilçi, N. & Peytcheva, I. (2021). Peritectic assemblage entrainment and mafic–felsic magma interaction in the Late Oligocene–Early Miocene Karadağ Pluton in the Biga Peninsula, northwest Turkey: petrogenesis and geodynamic implications. Turkish Journal of Earth Sciences, 30, 279-312.
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  • Biryol, B. C., Beck, S. L., Zandt, G. & Özacar, A. A. (2011). Segmented African lithosphere beneath the Anatolian region inferred from teleseismic P-wave tomography. Geophysical Journal International, 184(3), 1037-1057.
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  • Ersoy, Y. E., Helvacı, C., Uysal, İ., Karaoğlu, Ö., Palmer, M. R. & Dindi, F. (2012). Petrogenesis of the Miocene volcanism along the İzmir-Balıkesir Transfer Zone in western Anatolia, Turkey: Implications for origin and evolution of potassic volcanism in post-collisional areas. Journal of Volcanology and Geothermal Research, 241-242, 21-38.
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  • Kamacı, Ö. & Altunkaynak, Ş. (2020). The role of accreted continental crust in the formation of granites within the Alpine style continental collision zone: Geochemical and geochronological constrains from leucogranites in the Çataldağ Metamorphic Core Complex (NW Turkey). Lithos, 105347, 354–355.
  • Karacık, Z., Yılmaz, Y., Pearce, J. A. & Ece, O. I. (2008). Petrochemistry of the south Marmara granitoids, northwest Anatolia Turkey. International Journal of Earth Sciences, 97, 1181-1200.
  • Karaoğlu, O. & Helvacı, C. (2014). Isotopic evidence for a transition from subduction to slab-tear related volcanism in western Anatolia, Turkey. Lithos, 192-195, 226-239.
  • Krushensky, R. D. (1976). Neogene calc-alkaline extrusive and intrusive rocks of the Karalar Yeşiller area, Northwest Anatolia, Turkey. Bulletin Volcanologique, 39(2), 336-360.
  • Lambert, R. J. & Holland, J. G. (1974). Yttrium geochemistry applied to petrogenesis utilizing calcium-yttrium relationships in minerals and rocks. Geochima Cosmochima Acta, 38(9), 1393-1414.
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  • Le Maitre, R. W., Streckeisen, A., Zanettin, B., Le Bas, M. J., Bonin, B., Bateman, P., Bellieni, G., Dudek, A., Efremova, S., Keller, J., Lamere, J., Sabine, P. A., Schmid, R., Sorensen, H. & Woolley, A. R. (2002). Igneous rocks: A classification and glossary of terms, recommendations of the international union of geological sciences, subcommission of the systematics of igneous rocks. Cambridge University Press, Cambridge.
  • Lindsley, D. H. (1983). Pyroxene thermometry. American Mineralogist, 68(5-6), 477-493.
  • Lindsley, D. H. ve Andersen, D. J., 1983. A twopyroxene thermometer. Journal of Geophysical Research, 88, 887-906.
  • Luhr, J. F., Carmichael, I. S. E. & Varekamp, J. C. (1984). The 1982 eruptions of El Chicón Volcano, Chiapas, Mexico: Mineralogy and petrology of the anhydrite-bearing pumices. Journal of Vocanology and Geothermal Research, 23(1-2), 69-108.
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  • Morimoto, M. J., Fabries, A. K., Ferguson, I. V., Ginzburg, M. & Ross, F. A. (1988). Nomenclature of pyroxenes. Mineralogical Magazine, 52, 535-550.
  • Nachit, H., Ibhi, A., Abia, E. A. & Ohoud, M. B. (1985). Discrimination between primary magmatic biotites, reequilibrated biotites and neoformed biotites. Comptes Rendus Geoscience, 337(16), 1415-1420.
  • Okay, A. I. (2008). Geology of Turkey: a synopsis. Anschnitt, 21, 19-42.
  • Okay, A.I. & Tüysüz, O. (1999). Tethyan sutures of northern Turkey. In: Durant, B., Jolivet, F., Horvath, F. & Seranne, M. (Eds.), The Mediterranean basin: Tertiary extension within the Alpine orogen. Geological Society Special Publication, 156(1), 475-515.
  • Okay, A. I. & Satır, M. (2000). Upper Cretaceous eclogite – facies metamorphic rocks from the Biga peninsula, northwest Turkey. Turkish Journal Earth Sciences, 9, 47-56.
  • Okay, A. I., Tansel, I. & Tüysüz, O. (2001). Obduction, subduction and collision as reflected in the Upper Cretaceous–Lower Eocene sedimentary record of western Turkey. Geological Magazine, 138(2), 117-42.
  • Okay, A. I., Satır, M., Maluski, H., Siyako, M., Metzger, R. & Akyüz, S. (1996). Paleo-and Neo-Tethyan events in Northwest Turkey: geological and geochronological constrains. In: Yin, A. & Harrison, T. M. (Eds.), The tectonic evolution of Asia, (p. 420-444). Cambridge University Press, Cambridge.
  • Özgenç, İ. & İlbeyli, N. (2008). Petrogenesis of the Late Cenozoic Eğrigöz Pluton in Western Anatolia, Turkey: Implications for magma genesis and crustal processes. International Geology Review, 50, 375-391.
  • Pearce, J. A. (1983). The role of sub-continental lithosphere in magma genesis at destructive plate margins. In: Hawksworth, C. J. & Norry, M. J. (Eds.), Continental basalts and mantle xenoliths (pp. 230-249). Shiva, Nantwich.
  • Pearce, J. A. (1996). A user’s guide to basalt discrimination diagrams. In: Wyman, D. A. (Eds.), Trace element geochemistry of volcanic rocks: Applications for massive sulphide exploration: Winnipeg. Geological Association of Canada, Short Course Notes 12, 79-113.
  • Pearce, J. A. & Peate, D. W. (1995). Tectonic implications of the composition of volcanic arc magmas. Annual Review Earth Planet Sciences Letter, 23, 251-285.
  • Pearce, J. A., Bender, J. F., De Long, S. E., Kidd, W. S. F., Low, P. J., Güner, Y., Şaroğlu, F., Yılmaz, Y, Moorbath, S. & Mitchell, J. J. (1990). Genesis of collision volcanism in eastern Anatolia Turkey. Journal Volcanology Geotherm Research, 44(1-2), 189-229.
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  • Prelevic, D., Akal, C., Foley, S. F., Romer, R. L., Stracke, A. & Van Den Bogaard, P. (2012). Ultrapotassic mafic rocks as geochemical proxies for postcollisional dynamics of orogenic lithospheric mantle: the case of southwestern Anatolia, Turkey. Journal of Petrology, 53(5), 1019-1055.
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  • Saatcı, E. S. & Aslan, Z. (2018). Petrography and petrology of the Yürekli (Balıkesir) volcanics: an example of post-collisional felsic volcanism in the Biga peninsula (NW Turkey). Bulletin of the Mineral Research and Exploration, 157, 103-120.
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  • Topuz, G. & Okay, A.I. (2017). Late Eocene–Early Oligocene two-mica granites in NW Turkey (the Uludağ Massif): Water-fluxed melting products of a mafic metagreywacke. Lithos, 268–271, 334–350
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  • Uchida, E., Endo, S. & Makino, M. (2007). Relationship between solidifi cation depth of granitic rocks and formation of hydrothermal ore deposits. Resource Geology, 57(1), 47–56.
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  • Yılmaz, Y. (1990). Comparison of young volcanic associations of western and eastern Anatolia under compressional regime; a review. Journal of Volcanology and Geothermal Research, 44(1), 69-87.
  • Yılmaz, Y., Genç, S. C., Karacik, Z. & Altunkaynak, Ş. (2001). Two contrasting magmatic associations of NW Anatolia and their tectonic significance. Journal of Geodynamics, 31(3), 243-271.
  • Wilson, F. H. (1989). Geologic setting, petrology and age of Plicene to Holocene volcanoes of the stepovak Bay area, western Alaska Peninsula. In Dover, J. H. & Galloway, J. P. (Eds.), Geological studies in Alaska by the U.S. Geological Survey. United State Geological Survey Bulletin, 1903, 84-95.
  • Wones, D. R. (1989). Significance of the assemblage titanite+magnetite+quartz in granitic rocks. American Mineralogist, 74(7-8), 744-749.
  • Zellmer, G. F., Annen, C., Charlier, B. L. A., George, R. M. M., Turner, S. P. & Hawkesworth, C. J.(2005). Magma evolution and ascent at volcanic arcs: Constraining petrogenetic processes through rates and chronologies. Journal of Volcanology and Geothermal Research, 140, 171-191.
  • Zhu, D. C., Pan, G. T., Mo, X. X., Liao, Z. L., Jiang, X. S., Wang, L. Q. & Zhao, Z. (2007). Petrogenesis of volcanic rocks in the Sangxiu Formation, central segment of Tethyan Himalaya: A probable example of plume–lithosphere interaction. Journal of Asian Earth Science, 29(2), 320-335.
Toplam 73 adet kaynakça vardır.

Ayrıntılar

Birincil Dil Türkçe
Konular Mineraloji-Petrografi
Bölüm Makaleler - Articles
Yazarlar

Ferhat Bozan Bu kişi benim 0000-0001-9039-520X

Zafer Aslan 0000-0002-3418-4368

Proje Numarası Proje No: 2018/049
Yayımlanma Tarihi 15 Nisan 2022
Gönderilme Tarihi 3 Kasım 2021
Kabul Tarihi 22 Ocak 2022
Yayımlandığı Sayı Yıl 2022 Cilt: 65 Sayı: 2

Kaynak Göster

APA Bozan, F., & Aslan, Z. (2022). Büyükbostancı-Çiçekpınar (Balıkesir, KB Türkiye) Yöresindeki Oligosen-Miyosen Yaşlı Kalk-alkalen Volkanik Kayaçların Mineral Kimyası, Jeokimyası ve Petrolojisi. Türkiye Jeoloji Bülteni, 65(2), 117-148. https://doi.org/10.25288/tjb.1018440
AMA Bozan F, Aslan Z. Büyükbostancı-Çiçekpınar (Balıkesir, KB Türkiye) Yöresindeki Oligosen-Miyosen Yaşlı Kalk-alkalen Volkanik Kayaçların Mineral Kimyası, Jeokimyası ve Petrolojisi. Türkiye Jeol. Bült. Nisan 2022;65(2):117-148. doi:10.25288/tjb.1018440
Chicago Bozan, Ferhat, ve Zafer Aslan. “Büyükbostancı-Çiçekpınar (Balıkesir, KB Türkiye) Yöresindeki Oligosen-Miyosen Yaşlı Kalk-Alkalen Volkanik Kayaçların Mineral Kimyası, Jeokimyası Ve Petrolojisi”. Türkiye Jeoloji Bülteni 65, sy. 2 (Nisan 2022): 117-48. https://doi.org/10.25288/tjb.1018440.
EndNote Bozan F, Aslan Z (01 Nisan 2022) Büyükbostancı-Çiçekpınar (Balıkesir, KB Türkiye) Yöresindeki Oligosen-Miyosen Yaşlı Kalk-alkalen Volkanik Kayaçların Mineral Kimyası, Jeokimyası ve Petrolojisi. Türkiye Jeoloji Bülteni 65 2 117–148.
IEEE F. Bozan ve Z. Aslan, “Büyükbostancı-Çiçekpınar (Balıkesir, KB Türkiye) Yöresindeki Oligosen-Miyosen Yaşlı Kalk-alkalen Volkanik Kayaçların Mineral Kimyası, Jeokimyası ve Petrolojisi”, Türkiye Jeol. Bült., c. 65, sy. 2, ss. 117–148, 2022, doi: 10.25288/tjb.1018440.
ISNAD Bozan, Ferhat - Aslan, Zafer. “Büyükbostancı-Çiçekpınar (Balıkesir, KB Türkiye) Yöresindeki Oligosen-Miyosen Yaşlı Kalk-Alkalen Volkanik Kayaçların Mineral Kimyası, Jeokimyası Ve Petrolojisi”. Türkiye Jeoloji Bülteni 65/2 (Nisan 2022), 117-148. https://doi.org/10.25288/tjb.1018440.
JAMA Bozan F, Aslan Z. Büyükbostancı-Çiçekpınar (Balıkesir, KB Türkiye) Yöresindeki Oligosen-Miyosen Yaşlı Kalk-alkalen Volkanik Kayaçların Mineral Kimyası, Jeokimyası ve Petrolojisi. Türkiye Jeol. Bült. 2022;65:117–148.
MLA Bozan, Ferhat ve Zafer Aslan. “Büyükbostancı-Çiçekpınar (Balıkesir, KB Türkiye) Yöresindeki Oligosen-Miyosen Yaşlı Kalk-Alkalen Volkanik Kayaçların Mineral Kimyası, Jeokimyası Ve Petrolojisi”. Türkiye Jeoloji Bülteni, c. 65, sy. 2, 2022, ss. 117-48, doi:10.25288/tjb.1018440.
Vancouver Bozan F, Aslan Z. Büyükbostancı-Çiçekpınar (Balıkesir, KB Türkiye) Yöresindeki Oligosen-Miyosen Yaşlı Kalk-alkalen Volkanik Kayaçların Mineral Kimyası, Jeokimyası ve Petrolojisi. Türkiye Jeol. Bült. 2022;65(2):117-48.
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