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《Geoscience》 2014-01
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LA-ICP-MS U-Pb Geochronology,Petrogenesis and Its Geological Implications of Kungeyite Plutons in Southern Altay Orogenic Belt

ZHANG Ya-feng;LIN Xin-wang;WANG Xing;GUO Qi-ming;ZHAO Duan-chang;L Jun-li;WANG Xu;Shaanxi Center of Geological Survey;Xi'an Institute of Geological and Mineral Exploration;  
The Kungeyite plutons,outcropped in Qingeli River in Qinghe County of southern margin of Altay orogenic belt are mainly hornblende biotite tonalite,which were determined for LA-ICP-MS zircon U-Pb ages. The result shows that the zircon206Pb /238U weighted average age is( 403. 4 ± 7. 4) Ma( MSWD = 1. 07),indicating the plutons were formed at Early Devonian. The SiO2contents range from 52. 39% to 71. 89% and σ from 0. 68 to 1. 53,A / CNK from 0. 76 to 1. 06,indicating that the plutons are mid-K calc-alkaline,metaluminous-weakly peraluminous rocks. In addition,the plutons are enrichment in LILE( Cs,Rb,Th,U) and LREE,obvious negative anomaly in HFSE( Nb,Ta,Hf,Ti),HREE and Eu( δEu = 0. 56-0. 86),thus resembling granitoid rocks formed in island-arc. Combined with the data of southern margin of Altay,the Kungeyite plutons were generated by partial melting of the lower crust underplayed by mafic magma of the mantle in a continental arc setting of active continental margin,and occurred magma mixing and differentiation.
【Fund】: 中国地质调查局区域地质调查项目(1212011120503 1212011120509)
【CateGory Index】: P588.122;P597.3
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