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

Year 2022, Volume: 65 Issue: 2, 117 - 148, 15.04.2022

Ferhat Bozan Zafer Aslan

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

Abstract

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.

Keywords

Andesite Biga Peninsula Hallaçlar Volcanic Rocks geochemistry mineral chemistry

Project Number

Proje No: 2018/049

References

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

Year 2022, Volume: 65 Issue: 2, 117 - 148, 15.04.2022

Ferhat Bozan Zafer Aslan

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

Abstract

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.

Keywords

Andezit Biga Yarımadası Hallaçlar Volkanik Kayaçları jeokimya mineral kimyası

Supporting Institution

Balıkesir Üniversitesi Bilimsel Araştırma Projeler Birimi

Project Number

Proje No: 2018/049

Thanks

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

References

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  • 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.
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  • 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.
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There are 73 citations in total.

Details

Primary Language Turkish
Subjects Mineralogy- Petrography
Journal Section Makaleler - Articles
Authors

Ferhat Bozan This is me 0000-0001-9039-520X

Zafer Aslan 0000-0002-3418-4368

Project Number Proje No: 2018/049
Publication Date April 15, 2022
Submission Date November 3, 2021
Acceptance Date January 22, 2022
Published in Issue Year 2022 Volume: 65 Issue: 2

Cite

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. Geol. Bull. Turkey. April 2022;65(2):117-148. doi:10.25288/tjb.1018440
Chicago Bozan, Ferhat, and Zafer Aslan. “Büyükbostancı-Çiçekpınar (Balıkesir, KB Türkiye) Yöresindeki Oligosen-Miyosen Yaşlı Kalk-Alkalen Volkanik Kayaçların Mineral Kimyası, Jeokimyası Ve Petrolojisi”. Türkiye Jeoloji Bülteni 65, no. 2 (April 2022): 117-48. https://doi.org/10.25288/tjb.1018440.
EndNote Bozan F, Aslan Z (April 1, 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 and Z. Aslan, “Büyükbostancı-Çiçekpınar (Balıkesir, KB Türkiye) Yöresindeki Oligosen-Miyosen Yaşlı Kalk-alkalen Volkanik Kayaçların Mineral Kimyası, Jeokimyası ve Petrolojisi”, Geol. Bull. Turkey, vol. 65, no. 2, pp. 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 (April 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. Geol. Bull. Turkey. 2022;65:117–148.
MLA Bozan, Ferhat and Zafer Aslan. “Büyükbostancı-Çiçekpınar (Balıkesir, KB Türkiye) Yöresindeki Oligosen-Miyosen Yaşlı Kalk-Alkalen Volkanik Kayaçların Mineral Kimyası, Jeokimyası Ve Petrolojisi”. Türkiye Jeoloji Bülteni, vol. 65, no. 2, 2022, pp. 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. Geol. Bull. Turkey. 2022;65(2):117-48.
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