| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4731806 | Journal of Asian Earth Sciences | 2011 | 23 Pages |
Abstract
Variation of several major oxide concentrations (Fe2O3, TiO2, CaO and K2O), trace element concetrations (V, Sr, Cs and Rb) and trace element ratios (Ba/Rb, Sr/, K/Sr, K/Nb, Rb/Sr, Rb/Y and Rb/Nb) versus SiO2 concentration show the magma chamber that generated the Incesu ignimbrite was compositionally zoned. All geochemical and Sr-Nd isotpic datas can be interepreted to be the result of a subduction related source.
Related Topics
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Authors
Tamer Koralay, Yusuf KaÄan Kadioglu, Peter Davis,