Petrogenesis of the late Cretaceous Turnagoel intrusion in the eastern Pontides: Implications for magma genesis in the arc setting |
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引用本文: | Abdullah Kaygusuz,Ferkan Sipahi,Nurdane Ilbeyli,Mehmet Arslan,Bin Chen,Emre Aydinakir.Petrogenesis of the late Cretaceous Turnagoel intrusion in the eastern Pontides: Implications for magma genesis in the arc setting[J].地学前缘(英文版),2013,4(4):423-438. |
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作者姓名: | Abdullah Kaygusuz Ferkan Sipahi Nurdane Ilbeyli Mehmet Arslan Bin Chen Emre Aydinakir |
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作者单位: | Department,of Geological Engineering.Gmshane University;Department of Geological Engineering,Akdeniz University;Department,of Geological Engineering.Karadeniz Technical University;Department of Geological Engineering.Peking University;Department of Geological Engineering,Gmshane University |
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摘 要: | A series of Cretaceous plutons is present in the eastern Pontides of northeastern Turkey.The Turnagl intrusion is the least studied and,thus,the least understood plutons in the orogen.This intrusion consists of hornblende-biotite granodiorites emplaced at 78 Ma based on LA-ICP-MS U-Pb zircon dating.It is of sub- alkaline affinity,belongs to the medium- to high-K calc-alkaline series,and displays features typical of Itype granites.The rocks of the intrusion are enriched in large-ion lithophile elements and light rare earthelements with negative Eu anomalies(Eu/Eu*= 0.69-0.82),but are deficient in high-field-strength elements.They have a small range of (87Sr/86Sr)i(0.7060-0.7063),εNdi(-2.6 to -3.1),and δ18O(+8.1 to +9.1) values.Their Pb isotopic ratios are 206Pb/204Pb = 18.63-18.65,207Pb/204Pb = 15.62-15.63,and 208Pb/204Pb = 38.53-38.55.The fractionation of plagioclase,hornblende,and Fe-Ti oxides had key functions in the evolution of the Tumagl intrusion.The crystallization temperatures of the melts ranged from 758 to 885℃ as determined by zircon and apatite saturation thermometry.All these characteristics,combined with the low values of K2O/Na2O and(Na2O + K2O)/(FeOt+MgO + TiO2),as well as the high values of (CaO + FeOt + MgO + TiO2).suggest an origin by dehydration melting from a metabasaltic lowercrustal source.
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关 键 词: | Turnagl intrusion Late Cretaceous Sr-Nd-Pb-O isotope U-Pb zircon dating Eastern Pontides Turkey |
收稿时间: | 3 July 2012 |
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