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Mineral chemistry, whole-rock geochemistry and petrology of Eocene I-type shoshonitic plutons in the Gölköy area (Ordu, NE Turkey)

Yıl 2018, Cilt: 157 Sayı: 157, 121 - 152, 15.12.2018
https://doi.org/10.19111/bulletinofmre.371623

Öz

The Eocene intermediate to felsic plutons are widespread in varying sizes and compositions throughout the Eastern Pontides Orogenic Belt in NE Turkey. Of these, two monzonitic bodies (namely the Eriko Tepe and Göl Tepe Plutons) in the Gölköy (Ordu) area, extend nearly in the orientation of NW-SE and E-W and were emplaced into the Upper Cretaceous and/or Eocene volcanic and sedimentary rocks. Petrographically, the studied monzonitic plutons are compositionally fine to medium grained monzonite, monzodiorite and subordinate quartz-monzonite. They consist of plagioclase (An35-67), K-feldspar (Or61-96), quartz, clinopyroxene (Wo28-49En35-51Fs10-25), biotite (Mg#: 0.53-0.73) ± hornblende (Mg#: 0.65-0.82), Fe-Ti oxide with monzonitic, poikilitic, perthitic, rare antirapakivi and graphic textures. Mineral thermobarometer estimations imply that the plutons were crystallized in P-T conditions of mid to shallow crustal levels. Petrochemically, these monzonitic plutons show post-collisional, I-type, metaluminous (A/CNK=0.76-0.93) and shoshonitic features. The whole-rock major oxide and trace element variations suggest that fractionational crystallization played a significant role in the evolution of these monzonitic plutons. The primitive mantle-normalized trace element patterns of the studied plutons are similar to each other with enrichment in large ion lithophile elements, Th, Ce and negative Nb and Ti anomalies. Moreover, the chondrite-normalized rare earth element plots of the plutons show moderately enriched concave-shaped patterns (LaN/LuN=9.3-12.6) with negative Eu anomalies (EuN/Eu*=0.69-0.84), all of which imply plagioclase and clinopyroxene ± hornblende fractionations during their evolution. The geochemical data suggest that the monzonitic plutons have evolved from parental magmas derived from the melts of enriched lithospheric mantle in a post-collisional setting.

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Mineral chemistry, whole-rock geochemistry and petrology of Eocene I-type shoshonitic plutons in the Gölköy area (Ordu, NE Turkey)

Yıl 2018, Cilt: 157 Sayı: 157, 121 - 152, 15.12.2018
https://doi.org/10.19111/bulletinofmre.371623

Öz

The Eocene intermediate to felsic plutons are widespread in varying sizes and compositions throughout the Eastern Pontides Orogenic Belt in NE Turkey. Of these, two monzonitic bodies (namely the Eriko Tepe and Göl Tepe Plutons) in the Gölköy (Ordu) area, extend nearly in the orientation of NW-SE and E-W and were emplaced into the Upper Cretaceous and/or Eocene volcanic and sedimentary rocks. Petrographically, the studied monzonitic plutons are compositionally fine to medium grained monzonite, monzodiorite and subordinate quartz-monzonite. They consist of plagioclase (An35-67), K-feldspar (Or61-96), quartz, clinopyroxene (Wo28-49En35-51Fs10-25), biotite (Mg#: 0.53-0.73) ± hornblende (Mg#: 0.65-0.82), Fe-Ti oxide with monzonitic, poikilitic, perthitic, rare antirapakivi and graphic textures. Mineral thermobarometer estimations imply that the plutons were crystallized in P-T conditions of mid to shallow crustal levels. Petrochemically, these monzonitic plutons show post-collisional, I-type, metaluminous (A/CNK=0.76-0.93) and shoshonitic features. The whole-rock major oxide and trace element variations suggest that fractionational crystallization played a significant role in the evolution of these monzonitic plutons. The primitive mantle-normalized trace element patterns of the studied plutons are similar to each other with enrichment in large ion lithophile elements, Th, Ce and negative Nb and Ti anomalies. Moreover, the chondrite-normalized rare earth element plots of the plutons show moderately enriched concave-shaped patterns (LaN/LuN=9.3-12.6) with negative Eu anomalies (EuN/Eu*=0.69-0.84), all of which imply plagioclase and clinopyroxene ± hornblende fractionations during their evolution. The geochemical data suggest that the monzonitic plutons have evolved from parental magmas derived from the melts of enriched lithospheric mantle in a post-collisional setting.

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  • Yücel, C. 2013. Trabzon-Giresun arasındaki Tersiyer volkanitlerinin petrografisi, 40Ar-39Ar jeokronolojisi, petrokimyası, Sr-Nd-Pb izotop jeokimyası ve petrolojisi. Doktora Tezi, KTÜ Fen Bilimleri Enstitüsü, 406p, Trabzon (unpublished).
  • Yücel, C., Arslan, M., Temizel, İ., Abdioğlu, E., Ruffet, G. 2012. Trabzon- Giresun Arasındaki Tersiyer Alkalen Volkanitlerinin Tüm-Kayaç Petrokimyası ve 40Ar-39Ar Jeokronolojisi, KD Türkiye. 65. Türkiye Jeoloji Kurultayı Bildiri Özleri Kitabı (Abstracts) pp.354-355.
  • Yücel, C., Arslan, M., Temizel, İ., Abdioğlu, E. 2014. Volcanic facies and mineral chemistry of Tertiary volcanics in the northern part of the Eastern Pontides, northeast Turkey: Implications for pre-eruptive crystallization conditions and magma chamber processes. Mineralogy and Petrology 108, pp.439-467.
  • Yücel, C., Arslan, M., Temizel, İ., Abdioğlu, E., Ruffet, G. 2017. Evolution of K-rich magmas derived from a net veined lithospheric mantle in an ongoing extensional setting: Geochronology and geochemistry of Eocene and Miocene volcanic rocks from Eastern Pontides (Turkey). Gondwana Research 45, pp.65-86.
Toplam 216 adet kaynakça vardır.

Ayrıntılar

Birincil Dil İngilizce
Konular Mühendislik
Bölüm Makaleler
Yazarlar

İrfan Temizel 0000-0002-6293-8649

Emel Abdioğlu Yazar

Mehmet Arslan

Abdullah Kaygusuz

Zafer Aslan

Yayımlanma Tarihi 15 Aralık 2018
Yayımlandığı Sayı Yıl 2018 Cilt: 157 Sayı: 157

Kaynak Göster

APA Temizel, İ., Abdioğlu Yazar, E., Arslan, M., Kaygusuz, A., vd. (2018). Mineral chemistry, whole-rock geochemistry and petrology of Eocene I-type shoshonitic plutons in the Gölköy area (Ordu, NE Turkey). Bulletin of the Mineral Research and Exploration, 157(157), 121-152. https://doi.org/10.19111/bulletinofmre.371623
AMA Temizel İ, Abdioğlu Yazar E, Arslan M, Kaygusuz A, Aslan Z. Mineral chemistry, whole-rock geochemistry and petrology of Eocene I-type shoshonitic plutons in the Gölköy area (Ordu, NE Turkey). Bull.Min.Res.Exp. Aralık 2018;157(157):121-152. doi:10.19111/bulletinofmre.371623
Chicago Temizel, İrfan, Emel Abdioğlu Yazar, Mehmet Arslan, Abdullah Kaygusuz, ve Zafer Aslan. “Mineral Chemistry, Whole-Rock Geochemistry and Petrology of Eocene I-Type Shoshonitic Plutons in the Gölköy Area (Ordu, NE Turkey)”. Bulletin of the Mineral Research and Exploration 157, sy. 157 (Aralık 2018): 121-52. https://doi.org/10.19111/bulletinofmre.371623.
EndNote Temizel İ, Abdioğlu Yazar E, Arslan M, Kaygusuz A, Aslan Z (01 Aralık 2018) Mineral chemistry, whole-rock geochemistry and petrology of Eocene I-type shoshonitic plutons in the Gölköy area (Ordu, NE Turkey). Bulletin of the Mineral Research and Exploration 157 157 121–152.
IEEE İ. Temizel, E. Abdioğlu Yazar, M. Arslan, A. Kaygusuz, ve Z. Aslan, “Mineral chemistry, whole-rock geochemistry and petrology of Eocene I-type shoshonitic plutons in the Gölköy area (Ordu, NE Turkey)”, Bull.Min.Res.Exp., c. 157, sy. 157, ss. 121–152, 2018, doi: 10.19111/bulletinofmre.371623.
ISNAD Temizel, İrfan vd. “Mineral Chemistry, Whole-Rock Geochemistry and Petrology of Eocene I-Type Shoshonitic Plutons in the Gölköy Area (Ordu, NE Turkey)”. Bulletin of the Mineral Research and Exploration 157/157 (Aralık 2018), 121-152. https://doi.org/10.19111/bulletinofmre.371623.
JAMA Temizel İ, Abdioğlu Yazar E, Arslan M, Kaygusuz A, Aslan Z. Mineral chemistry, whole-rock geochemistry and petrology of Eocene I-type shoshonitic plutons in the Gölköy area (Ordu, NE Turkey). Bull.Min.Res.Exp. 2018;157:121–152.
MLA Temizel, İrfan vd. “Mineral Chemistry, Whole-Rock Geochemistry and Petrology of Eocene I-Type Shoshonitic Plutons in the Gölköy Area (Ordu, NE Turkey)”. Bulletin of the Mineral Research and Exploration, c. 157, sy. 157, 2018, ss. 121-52, doi:10.19111/bulletinofmre.371623.
Vancouver Temizel İ, Abdioğlu Yazar E, Arslan M, Kaygusuz A, Aslan Z. Mineral chemistry, whole-rock geochemistry and petrology of Eocene I-type shoshonitic plutons in the Gölköy area (Ordu, NE Turkey). Bull.Min.Res.Exp. 2018;157(157):121-52.

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