Araştırma Makalesi

Geochemistry and Mineralization Potential of the Ophiolitic Rocks in Konya Region

Cilt: 4 Sayı: 2 15 Aralık 2020
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Geochemistry and Mineralization Potential of the Ophiolitic Rocks in Konya Region

Öz

Geochemical studies performed in ophiolitic rocks and placers located in three different regions around Konya (Hatıp-Çayırbağı, Altınekin, Yükselen) show that the average Si and Al in both rocks and placers are lower than the earth crust. On the other hand, the average Fe, Cr, Mg, Co, Ni and Ti contents are higher than the average amounts in the earth's crust. While Cu content of Hatıp-Çayırbağı ophiolitic rocks are at high values, Pb and Zn contents are observed at high values in Altınekin region. While Cr2O3 in Hatıp-Çayırbağı region shows 5 times enrichment in placers compared to rocks, it shows approximately 4 times enrichment in Yükselen region. In the Altınekin region, Au shows five times more enrichment. Rare Earth Elements (REE) are highly enriched in all regions. According to the simple correlation and cluster analysis of the components analyzed in all three regions, it is revealed that the examined ophiolitic rocks were formed by similar processes.

Anahtar Kelimeler

Destekleyen Kurum

This study was supported by Selcuk University Scientific Research Projects Coordinator (Project No: 14401023).

Proje Numarası

Project No: 14401023

Teşekkür

We thank forever for the Coordination Office of Scientific Research Projects (BAP) of Selçuk University (BAP’s Project No: 14401023).

Kaynakça

  1. [1] Şengör, A.M.C., Yılmaz, Y., 1981. Tethyan evolution of Turkey: A plate tectonic approach. Tectonophysics, 75, 181–241.
  2. [2] Pearce, J.A., Lippard S.J., Roberts, S., 1984. Characteristics and tectonic significance of supra-subduction zone ophiolites, Geological Society, London, Special Publications, 16, 77-94.
  3. [3] Robertson, A.H.F., Dixon, J.E., 1984. Introduction: aspects of the geological evolution of the Eastern Mediterranean. In: Dixon, J.E., Robertson, A.H.F. (Eds.), The Geological Evolution of the Eastern Mediterranean. Geological Society of London Special Publication, 17, 1–74.
  4. [4] Parlak, O., Yılmaz, H., Boztuğ, D., 2006. Origin and tectonic significance of the metamorphic sole and isolated dikes of the Divriği Ophiolite (Sivas, Turkey): Evidence for slab break-off prior to ophiolite emplacement. Turkish Journal of Earth Sciences, 15, 25–45.
  5. [5] Furnes, H., Dilek, Y., Zhao, G., Safonova, I., Santosh, M., 2020. Geochemical characterization of ophiolites in the Alpine-Himalayan Orogenic Belt: Magmatically and tectonically diverse evolution of the Mesozoic Neotethyan oceanic crust, 208, 103258.
  6. [6] Dilek, Y., Furnes, H., 2009. Structure and geochemistry of Tethyan ophiolites and their petrogenesis in subduction rollback systems, Lithos, 113, 1–20.
  7. [7] Öztürk, A., Arık, F., and Özen, Y., 2016, Investigation in Terms of Formatıon, Genetic Relation and Ore Deposit of the Ophiolitic Rocks in Çayırbağı-Hatıp-Yükselen-Altınekin (Konya) Regions, Selçuk University Department of Geological Engineering, Project number: 14401023.
  8. [8] Patyk-Kara, N. G., Gorelikova, N. V., Bardeeva, E. G. and Shevelev, A. G., 2001, Mineralogy of Placers: Modern Approaches and Solutions, Lithology and Mineral Resources, Vol. 36, No. 5, 2001, pp. 393–405.

Ayrıntılar

Birincil Dil

İngilizce

Konular

Jeoloji (Diğer)

Bölüm

Araştırma Makalesi

Yayımlanma Tarihi

15 Aralık 2020

Gönderilme Tarihi

22 Kasım 2020

Kabul Tarihi

22 Aralık 2020

Yayımlandığı Sayı

Yıl 2020 Cilt: 4 Sayı: 2

Kaynak Göster

APA
Öztürk, A., Özen, Y., & Arık, F. (2020). Geochemistry and Mineralization Potential of the Ophiolitic Rocks in Konya Region. Uluslararası Çevresel Eğilimler Dergisi, 4(2), 93-109. https://izlik.org/JA57LG77SL
AMA
1.Öztürk A, Özen Y, Arık F. Geochemistry and Mineralization Potential of the Ophiolitic Rocks in Konya Region. IJENT. 2020;4(2):93-109. https://izlik.org/JA57LG77SL
Chicago
Öztürk, Alican, Yeşim Özen, ve Fetullah Arık. 2020. “Geochemistry and Mineralization Potential of the Ophiolitic Rocks in Konya Region”. Uluslararası Çevresel Eğilimler Dergisi 4 (2): 93-109. https://izlik.org/JA57LG77SL.
EndNote
Öztürk A, Özen Y, Arık F (01 Aralık 2020) Geochemistry and Mineralization Potential of the Ophiolitic Rocks in Konya Region. Uluslararası Çevresel Eğilimler Dergisi 4 2 93–109.
IEEE
[1]A. Öztürk, Y. Özen, ve F. Arık, “Geochemistry and Mineralization Potential of the Ophiolitic Rocks in Konya Region”, IJENT, c. 4, sy 2, ss. 93–109, Ara. 2020, [çevrimiçi]. Erişim adresi: https://izlik.org/JA57LG77SL
ISNAD
Öztürk, Alican - Özen, Yeşim - Arık, Fetullah. “Geochemistry and Mineralization Potential of the Ophiolitic Rocks in Konya Region”. Uluslararası Çevresel Eğilimler Dergisi 4/2 (01 Aralık 2020): 93-109. https://izlik.org/JA57LG77SL.
JAMA
1.Öztürk A, Özen Y, Arık F. Geochemistry and Mineralization Potential of the Ophiolitic Rocks in Konya Region. IJENT. 2020;4:93–109.
MLA
Öztürk, Alican, vd. “Geochemistry and Mineralization Potential of the Ophiolitic Rocks in Konya Region”. Uluslararası Çevresel Eğilimler Dergisi, c. 4, sy 2, Aralık 2020, ss. 93-109, https://izlik.org/JA57LG77SL.
Vancouver
1.Alican Öztürk, Yeşim Özen, Fetullah Arık. Geochemistry and Mineralization Potential of the Ophiolitic Rocks in Konya Region. IJENT [Internet]. 01 Aralık 2020;4(2):93-109. Erişim adresi: https://izlik.org/JA57LG77SL

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