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Geochemistry and Geochronology of Orthogneisses in the Derbent (Alaflehir) Area, Eastern Part of the Ödemifl–Kiraz Submassif, Menderes Massif: Pan-African Magmatic Activity
2004
Journal:  
Turkish Journal of Earth Sciences
Author:  
Abstract:

Menderes Masifi’nin Pan-Afrikan yafll› temel kayalar› ve Paleozoyik örtü serileri Ödemifl-Kiraz asmasifi’nin do¤usunda yer alan Derbent (Alaflehir) çevresinde yüzlek vermektedir. Pan-Afrikan temele ait granat-mika flistler, ortognayslar ve Triyas yafll› lökokratik ortognayslar›n ilksel kayalar› taraf›ndan intrüze olmufllard›r. Bu çal›flma, Proterozoyik sonunda Menderes Masifi’nin Pan-Afrikan evrimiyle iliflkili olan ortognayslar›n jeokimyas› ve jeokronolojisi üzerinedir. Jeokimyasal veriler ortognayslar›n S-tipli, peralumino ve kalkalkalen karakterli, sin-/posttektonik granitoyidlerden türedi¤ini göstermektedir. Ortognayslardan ayr›lan tipik magmatik ve öz flekilli zirkonlardan Pb-Pb evaporasyon yöntemiyle yafl tayinleri yap›lm›flt›r. ‹ki örne¤in tek zirkon 207Pb/206Pb yafllar› ortalama 561.5±1.8 my ve 570.5±2.2 my olarak elde edilmifltir. Bu yafllar ortognayslar›n ilksel kayalar›n›n sokulum yafl› olarak yorumlanm›flt›r. Menderes Masifi’ndeki bu ana magmatik olay okyanus havzalar›n›n kapanmas› ve Do¤u ve Bat› Gondvana’n›n çarp›flmas›na ba¤lant›l› Pan-Afrikan orojeneziyle iliflkilendirilebilir. 

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Turkish Journal of Earth Sciences

Field :   Fen Bilimleri ve Matematik

Journal Type :   Uluslararası

Metrics
Article : 773
Cite : 2.655
2023 Impact : 0.187
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Turkish Journal of Earth Sciences