The geology and mineralogical / petrographic features of Umurbabadag and its surroundings (Esme, Usak-Turkey)
Keywords:
brick, insulation, perlite Menderes Massif, Mineralogy/Petrography, General Geology, Eşme-Uşak
Abstract
Although numerous geological studies have been carried out in many regions of the Menderes Massif, even in areas close to the study area, no detailed geological mapping of the study area has been found. Within the scope of this study, geological, mineralogical-petrographic studies of Umurbabadağ and its vicinity were carried out and detailed 1/25,000 scaled geological mapping of the area was completed. When the findings obtained from the field and mineralogy-petrographic studies are compared with the general geological features of the Menderes Massif, it is understood that the study area is located within the Demirci-Gordes submassif of the Menderes Massif. Paragneisses (fine-grained gneisses) and orthogneisses having shear and/or compatible contact with these rocks belonging to the Latest Proterozoic-Earl Cambrian Core of the Menderes Massif crop out in the area. The fine-grained gneiss unit, corresponding to the Pan-African basement, outcrops in a very large area in the field. Amphibolite bodies, meta-aplite and meta leucogranites are present at different locations, generally cutting the fine-grained gneisses. Meta-aplite and meta leucogranites have been interpreted as granite porphyries of granitic augen gneisses, while amphibolites have been interpreted as basic magmatics cutting the Precambrian-Cambrian basement. The second widely observed rocks in the field is granitic augen gneisses (orthogneisses). These rocks are sometimes intermediate levels in fine-grained gneisses and sometimes cut the unit. As a result of the structural analysis performed on the metamorphic rocks in the area, it was observed that the main strike axes of the rocks are N40-50°E and the rocks are affected by a NW-SE trending force pair. It was concluded that the findings obtained were compatible with the properties agreed on the massif.
References
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[19] [19] Vural A, Corumluoglu O, Asri İ. Exploring Gördes Zeolite Sites by Feature Oriented Principle Component Analysis of LANDSAT Images. Caspian Journal of Environmental Sciences 2016; 14:285–298.
[20] Vural A. Soil geochemistry study of the listvenite area of Ayvacik (Çanakkale, Turkey). Caspian Journal of Environmental Sciences 2020; 18:205–215.
[21] Aydal D, Vural A, Taşdelen-Uslu İ, Aydal, Emine G. Crosta Technique Application On Bayramic (Alakeçi-Kısacık) Mineralized Area By Using Landsat 7 Etm+ Data. J FacEngArch Selcuk Univ 2007; 22:29–40.
[22] Vural A, Aydal D. Soil geochemical prospeting at lisvenite area, Bayramiç, (Çanakkale Turkey). 34th National and the 2nd International Geosciences Congress proceedings book. 22-24 Feb. 2016 Tehran, Iran. 2016.
[23] Vural A, Corumluoglu O, Asri I. Zeolitleşmelerin Uzaktan Algılama Metotlarıyla Tespit Edilmesi: Gördes (Manisa) Örneği. 14. Türkiye Harita Bilimsel ve Teknik Kurultayı. 2013.
[24] Aydal D, Vural A, Taşdelen-Uslu İ, Aydal, Emine G. Investigation of Kuşçayırı-Kartaldağı (Bayramiç-Çanakkale) mineral enhancement region by Crosta technique with LANDSAT 7 ETM+ bands. Technical University of İstanbul, First Remote Sensing Workshop and panel book, 11p in Turkish with English abstract. 2006.
[25] Vural A, Aydal D, Akpınar İ. A low sulphur epithermal gold mineralization in Kisacik-Ayvacik area (Çanakkale-Turkey). Goldschmidt Conference Abstracts. Prague, Czech Republic: 2011:2105.
[26] Vural A. Güneyköy ve Çevresi (Eşme-Uşak) Arsenopirit Cevherleşmelerinin Maden Jeolojisi/Mining Geology of Arsenopyrite Mineralizations in Güneyköy and Surroundings (Eşme-Uşak). Ankara University, 1998.
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[28] Vural A, Albayrak M. Geochemical and Mineralogical Properties of Zeolites from Gördes (Manisa) and Its Near Vicinity. 2nd International Conference on Engineering and Natural Sciences (ICENS 2016). 2016.
[29] Sönmez FN, Yılmaz H, Çiçek M, Koralay OE, Niedermann S, Kirk J. Age and source of the Küre/Ödemiş arsenopyrite-gold mineralization (Menderes Massif, Turkey) determined by Re-Os-He isotopes. Ore Geology Reviews 2020; 118:103333.
[30] Sönmez FN, Yılmaz H, Güngör T. Uşak/Eşme (Menderes Masifi) Sahasında Altın İçeren Arsenopirit-Kuvars Damarlarının Mineralojisi, Sıvı Kapanım ve Cevherleşme Yaşı (187Re/188Os) Üzerine Bir Çalışma. 67th Geological Congress of Turkey. Ankara, Turkey: 2014:522–523.
[31] Vural A, Çorumluoğlu Ö, Asri İ. Investigation of Litologic structures and Alterations in Hazine Cave and Dere Mine regions in Turkey by Remote Sensing Techniques. TUFUAB VI. Technical Symposium, 21th February, Antalya (in Turkish with English abstract). 2011.
[32] Corumluoglu O, Vural A, Asri I. Determination of Kula basalts (geosite) in Turkey using remote sensing techniques. Arabian Journal of Geosciences 2015; 8:10105–10117.
[33] Konak N, Akat U, Afşar ÖP, Akay E, Akçaören F, Akçay AE, Akçay Y, Akdeniz N, Akıncı H, Akkök R, Akyol Z, Akyürek B, et al. İzmir, 1/500 000’lik Jeoloji Haritası (Kompilasyon). Ankara, Türkiye: Maden Tetkik ve Arama Genel Müdürlüğü; 2002.
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Published
2020-12-31
How to Cite
Vural, A., & Unlu, T. (2020). The geology and mineralogical / petrographic features of Umurbabadag and its surroundings (Esme, Usak-Turkey). Journal of Engineering Research and Applied Science, 9(2), 1561-1587. Retrieved from http://journaleras.com/index.php/jeras/article/view/219
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