MANTO PERİDOTİTLERİNDE KISMİ ERGİME VE METAZOMATİZMA ETKİSİ: KIZILDAĞ OFİYOLİTİ ÖRNEĞİ (HATAY, TÜRKİYE)

Mustafa Eren Rizeli; A. Feyzi Bingol; Abdullah Sar; Kuo-lung Wang

doi:10.17780/ksujes.1437482

EN TR

PARTIAL MELTING AND METASOMATISM EFFECTS IN MANTLE PERIDOTITES: THE CASE OF KIZILDAĞ OPHIOLITE (HATAY, TURKEY)

Abstract

The Kızıldağ ophiolite is located in the SE Anatolian Ophiolite Belt and composed, from bottom to top, of mantle peridotites, mafic-ultramafic cumulates, isotropic gabbros, sheeted-dyke complex, plagiogranites and volcanic rocks. Based on detailed field studies and petrographic observations in mantle peridotites, selected samples' major oxide, trace, and REE contents were determined for the whole rock. The investigated rocks, generally composed of harzburgite and a small amount of dunite, display granoblastic and mesh textures. Rocks that have been depleted to different degrees compared to the composition of the primordial upper mantle have low Al2O3, CaO, TiO2, and high MgO contents. Enrichments in high-field strength elements and large ion lithophile elements are observed in some samples. Presence of orthopyroxenite channels cutting peridotites in the field; petrographically, secondary clinopyroxene formations, worm-like pyroxene-spinel symplectites, olivine inclusions within spinels; geochemically, trace element enrichments (Cs, Rb, Ti, Sr, Pb, Ce, Zr/Hf and Th/La) in some samples are a result of the metasomatism of aqueous fluids and melts derived from the subducted slab. As a result, Kızıldağ mantle peridotites are fore-arc peridotites that have been depleted by more than 20% and show evidence of metasomatism that characterizes the subduction zone environment.

Keywords

MANTO PERİDOTİTLERİNDE KISMİ ERGİME VE METAZOMATİZMA ETKİSİ: KIZILDAĞ OFİYOLİTİ ÖRNEĞİ (HATAY, TÜRKİYE)

Öz

Kızıldağ Ofiyoliti GD Anadolu Ofiyolit Kuşağı’nda yer alır ve tabandan tavana doğru manto peridotitleri, mafik/ultramafik kümülatlar, izotropik gabrolar, levha-dayk karmaşığı, plajiyogranitler ve volkanik kayaçlardan oluşmaktadır. Manto peridotitlerinde yapılan detaylı arazi çalışmaları ve petrografik gözlemler neticesinde seçilen örneklerin tüm kayaç ana oksit ve iz ve NTE içerikleri belirlenmiştir. Genellikle harzburjit ve az miktarda dünitten oluşan kayaçlar taneli ve elek dokular sergilemektedir. İlksel üst mantoya bileşimine kıyasla farklı derecelerde tüketilmiş olan kayaçlar; düşük Al2O3, CaO, TiO2 ve yüksek MgO içeriklerine sahiptir. Bazı örneklerde yüksek çekim alanlı elementler ve büyük iyon çaplı elementlerin bir kısmında zenginleşmeler görülmektedir. Arazide peridotitleri kesen ortopiroksenit kanallarının varlığı; petrografik olarak ikincil klinopiroksen oluşukları, kurtçuk şekilli (worm-like) piroksen-spinel simplektitler, olivinlerin spineller içinde kapanımı; jeokimyasal olarak bazı örneklerdeki iz element zenginleşmeleri (Cs, Rb, Ti, Sr, Pb, Ce, Zr/Hf ve Th/La) yiten levhadan türeyen sulu akışkanların ve ergiyiklerin metazomatizmasının bir sonucudur. Sonuç olarak Kızıldağ manto peridotitleri, %20’den fazla oranda tüketilmiş ve yitim zonu ortamını karakterize eden metazomatizma kanıtları gösteren yay önü peridotitleridir. .

Anahtar Kelimeler

Supporting Institution

TÜBİTAK

Project Number

117Y303

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Details

Primary Language

Turkish

Subjects

Mineralogy- Petrography

Journal Section

Research Article

Authors

Mustafa Eren Rizeli ^*
0000-0003-3725-3063
Türkiye

A. Feyzi Bingol
0000-0002-1767-1076
Türkiye

Abdullah Sar
0000-0002-9752-7807
Türkiye

Kuo-lung Wang
0000-0002-6447-2168
Taiwan

Publication Date

September 3, 2024

Submission Date

February 15, 2024

Acceptance Date

April 14, 2024

Published in Issue

Year 2024 Volume: 27 Number: 3

DOI

https://doi.org/10.17780/ksujes.1437482

IZ

https://izlik.org/JA48MF49BS

Cite

RIS / Bibtex

APA

Rizeli, M. E., Bingol, A. F., Sar, A., & Wang, K.- lung. (2024). MANTO PERİDOTİTLERİNDE KISMİ ERGİME VE METAZOMATİZMA ETKİSİ: KIZILDAĞ OFİYOLİTİ ÖRNEĞİ (HATAY, TÜRKİYE). Kahramanmaraş Sütçü İmam Üniversitesi Mühendislik Bilimleri Dergisi, 27(3), 908-928. https://doi.org/10.17780/ksujes.1437482