The Geological, Petrographical and Engineering Properties of Rhyolitic Tuffs (Çan Stone) in Çan-Etili Area (Çanakkale), NW Turkey: Their Usage as Building and Covering Stones
Oya Türkdönmez, Mustafa Bozcu
.
DOI: 10.4236/ojg.2012.21003   PDF    HTML     7,127 Downloads   13,668 Views   Citations

Abstract

In this study, the geological, petrographical properties of rhyolitic tuffs exposed around ?an-Etili in the Biga Peninsula (NW Turkey) which are pyroclastic products of Late Oligocene-Early Miocene aged ?an Volcanism were investigated, also physical and mechanical characteristics of tuffs introduced and tried to determine the impact on engineering properties of petrographical features. In the region, rhyolitic tuffs called locally “?an stone” have been used as covering and building stones for many years. These tuffs generally have light yellowish, beige, brown colored and different patterns with light yellowish, cream, reddish and brown colors caused by iron oxidation of hydrothermal alteration. They are preferred as coatings and decorative stone with these patterns. ?an stone which consisted of rhyolitic composition, lithic and locally crystalline tuffs has compact structure. The mineral assemblage of tuffs is mainly composed of quartz, plagioclase, rarely biotite, amphibole (hornblende) phenocrystals and opaque mineral with particles of volcanic glass and lithic fragments. Not only petrographical and geochemical analyses were carried out but also standard rock mechanic tests (unit weight, specific gravity, porosity, water absorption and uniaxial compressive strength) on rhyolitic tuffs samples collected from four different quarries (Hoppa Hill, Halilaga, Uzunalan, Dereoba). Simple regression analysis of test results obtained from four different regions and correlations were found good correlation between engineering proper- ties and the petrographical and chemical properties of rhyolitic tuffs.

Share and Cite:

O. Türkdönmez and M. Bozcu, "The Geological, Petrographical and Engineering Properties of Rhyolitic Tuffs (Çan Stone) in Çan-Etili Area (Çanakkale), NW Turkey: Their Usage as Building and Covering Stones," Open Journal of Geology, Vol. 2 No. 1, 2012, pp. 25-33. doi: 10.4236/ojg.2012.21003.

Conflicts of Interest

The authors declare no conflicts of interest.

References

[1] Y. Y?lmaz, “An Approach to the Origin of Young Volcanic Rocks of Western Turkey,” In: A. M. C. ?eng?r Ed., Tectonic Evolution of the Tethyan Region, Kliwer, Hague, 1989, pp. 159-189.
[2] Y. Y?lmaz, “Comparisons of the Young Volcanic Associations of the West and the East Anatolia under the Compressional Regime: A Review,” Journal of Volca- nology and Geothermal Research, Vol. 44, No. 1-2, 1990, pp. 69-87. doi:10.1016/0377-0273(90)90012-5
[3] Y. Y?lmaz, ?. C. Gen?, Z. Karac?k and ?. Altunkaynak, “Two Contrasting Magmatic Associations of NW Anatolia and Their Tectonic Significance,” Journal of Geody- namics, Vol. 31, No. 3, 2001, pp. 243-271. doi:10.1016/S0264-3707(01)00002-3
[4] O. Ertürk, E. Din??z and D. Alaygut, “Petrology of the Cenozoic Volcanics in the Biga Peninsula,” International Earth Saences Congress on Aegean Region Proceedings, II, NW Turkey, 1990, pp. 368-384.
[5] T. Ercan, M. Sat?r, G. Steinitz, A. Dora, E. Sar?fak?oglu, C. Adis, H. J. Walter and T. Y?ld?r?m, “Biga Yar?madas? ile G?k?eada, Bozcaada ve Tav?an Adalar?ndaki KB Anadolu Tersiyer Volkanizmas?n?n ?zellikleri (in Turkish),” MTA Dergisi, Vol. 117, 1995, pp. 55-86.
[6] E. Aldanmaz, J. Pearce, M. F. Thriwall, J. Mitchell, “Petro- genetic Evolution of Late Cenozoic, Post-Collison Volcanism in Western Anatolia, Turkey,” Journal of Volcanology and Geothermal Research, Vol. 102, No. 1-2, 2000, pp. 67-95. doi:10.1016/S0377-0273(00)00182-7
[7] ?. C. Gen?, M. D?nmez, A. Ak?ay and ?. Altunkaynak, “The Middle Eocene to Late Miocene Magmatic Evolution of the Biga Peninsula, NW Turkey,” 32nd International Geological Congress, Florence, 20-28 August 2004, p. 1298.
[8] ?. Altunkaynak and Y. Dilek, “Timing and Nature of Postcollisional Volcanism in Western Anatolia and Geodynamic Implications,” In: Y. Dilek and S. Pavlides, Eds., Post Collisional Tectonics and Magmatism in the Mediterranean Region and Asia, Geological Society of America Special Paper, Vol. 409, 2006, pp. 321-351.
[9] Y. Dilek and ?. Altunkaynak, “Cenozoic Crustal Evolution and Mantle Dynamics of Post-Collisional Magmatism in Western Anatolia,” International Geology Review, Vol. 49, No. 5, 2007, pp. 431-453. doi:10.2747/0020-6814.49.5.431
[10] ?. Altunkaynak and ?. C. Gen?, “Petrogenesis and Time- Progressive Evolution of the Cenozoic Continental Volcanism in the Biga Peninsula, NW Anatolia (Turkey),” Lithos, Vol. 102, No. 1-2, 2008, pp. 316-340. doi:10.1016/j.lithos.2007.06.003
[11] Y. Y?lmaz, “Ege B?lgesinde Gen? Magmatizman?n Olu- ?umu ile Litosferin Evrimi Aras?ndaki Ili?ki üzerine Dü?ünceler (in Turkish),” Jeofizik, Vol. 9, No. 10, 1995, pp. 107-110.
[12] N. K?prüba?? and E. Aldanmaz, “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, Vol. 46, No. 8, 2004, pp. 705-729. doi:10.2747/0020-6814.46.8.705
[13] T. Ercan, M. Sat?r, H. Kreuzer, A. Türkecan, E. Günay, A. ?evikba?, M. Ate? and B. Can, “Interpretation of New Chemical, Isotopic and Radiometric Data on Cenozoic Volcanics of Western Anatolia,” Bulletin of the Geological Society of Turkey, Vol. 28, 1985, pp. 121-136.
[14] E. Aldanmaz, N. Koprubas?, O. F. Gurer, N. Kaymakc? and A. Gourgaud, “Geochemical Constraints on the Cenozoic, OIB-Type Alkaline Volcanic Rocks of NW Turkey: Implications for Mantle Sources and Melting Processes,” Lithos, Vol. 86, No. 1-2, 2006, pp. 50-76.
[15] N. Güle?, “Crust-Mantle Interaction in Western Turkey: Implications from Sr to Nd Isotope Geochemistry of Tertiary and Quaternary Volcanics,” Geological Magazine, Vol. 128, No. 5, 1991, pp. 417-435.
[16] ?. Altunkaynak, “Collision-Driven Slab Breakoff Magmatism in Northwestern Anatolia,” Journal of Geology, Vol. 115, No. 1, 2007, pp. 63-82.
[17] TS 699, Do?al Yap? Ta?lar?-?nceleme ve Laboratuvar Deney Y?ntemleri, Türk Standardlar? Enstitüsü (TSE) (in Turkish), Ankara, 2009.
[18] P. Birkle and M. Sat?r, “Dating, Geochemistry and Geodynamic Significance of the Tertiary Magmatism of the Biga Peninsula, NW-Turkey, Geology of the Black Sea Region,” Mineral Research and Exploration Institute of Turkey, Ankara, 1995, pp. 171-180.
[19] N. B. ?ift?i, R, ?. Temel and M. N. Terzio?lu, “Neogene Stratigraphy and Hydrocarbon System of the Region Surrounding the Gulf of Edremit, NW Anatolia, Turkey,” TPJD Bulletin, Vol. 16, No. 2, 2004, pp. 81-104.
[20] M. Siyako, K. A. Burkan and A. I. ve Okay, “Biga ve Gelibolu Yar?madalar? Tersiyer Jeolojisi ve Hidrokarbon olanaklar?,” Turkish Association of Petroleum Geologist Bulletin, Vol. 1, 1989, pp. 183-199.
[21] M. J. Le Bas, R. W. Le Maitre, A. Streckeisen and B. Za- nettin, “A Chemical Classification of Volcanic Rocks Based on the Total Alkali-Silica Diagram,” Journal of. Petrology, Vol. 27, No. 3, 1986, pp. 445-450.
[22] H. Akda?, M. R. Bozkurt and T. D?kduran, “?anta??- Desenli Yap?ta?? (in Turkish): Turkey III,” Marble Symposium Proceedings, Turkey, 2001, pp. 153-162.
[23] O. ?im?ek and M. Erdal, “Investigation of Some Mechanical and Physical Properties of the Ahlat Stone (Ignimbrite) (in Turkish),” Journal of Science, Vol. 17, No. 4, 2004, pp. 71-78.
[24] M. Korkan?, “The Effect of Geomechanical Properties of ?gnimbrites on Their Usage as Building Stone: Nev?ehir Stone (in Turkish),” Geological Engineering, Vol. 31, No. 1, 2007, pp. 49-60.
[25] E. Yasar, A. Tolgay and A. Teymen, “Industrial Usage of Nevsehir-Kayseri (Turkey) Tuff Stone,” World Applied Sciences Journal, Vol. 7, No. 3, 2009, pp. 271-284.

Copyright © 2024 by authors and Scientific Research Publishing Inc.

Creative Commons License

This work and the related PDF file are licensed under a Creative Commons Attribution 4.0 International License.