Petrogenesis of the Late Cenozoic Egrigoz pluton in western Anatolia, Turkey: implications for magma genesis and crustal processes
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Dosyalar
Tarih
2008
Yazarlar
Dergi Başlığı
Dergi ISSN
Cilt Başlığı
Yayıncı
Taylor & Francis Inc
Erişim Hakkı
info:eu-repo/semantics/closedAccess
Özet
The western Anatolian magmatic province is typified by a large number of Late Cenozoic post-collisional granitoids. Of these magmatics, the Egrigoz pluton is one of the largest and least-understood plutons in the Menderes Massif. The Egrigoz intrusives are subalkaline, high-K, and calc-alkaline, and have characteristics of I-type granites. They consist mainly of granodiorite and granite. The intrusive rocks show enrichment in LILE and LREE relative to HFSE. Their chondrit-enormalized REE patterns are fractionated and have small negative Eu anomalies. Geochemical characteristics of the Egrigoz pluton indicate an origin through partial melting of mafic lower-crustal source rocks. In western Anatolia, the melt generation mechanism for the intrusive rocks could be crustal extension and uplift following collision.
Açıklama
Anahtar Kelimeler
Southern Menderes Massif, I-Type Granitoids, Core-Complex, Geochemical Constraints, Northwestern Anatolia, Tectonic Significance, Geodynamic Evolution, Continental-Crust, Augen Gneisses, Sw Turkey
Kaynak
International Geology Review
WoS Q Değeri
Q2
Scopus Q Değeri
Q1
Cilt
50
Sayı
4
