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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2017-01
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Chronological and geochemical characteristics and tectonic significance of Huoremudeke granitic pluton in Altay area of Xinjiang,China

TIAN Hongbiao;CHEN Youxin;HE Junling;ZENG Xiangwu;BAI Xiang;China University of Geosciences;No.8 Gold Geological Party of Chinese People's Armed Police Force;School of Earth Science and Resources,Chang'an University;  
The Huoremudeke granitic pluton occurs in the central part of the Altay Orogenic Belt(AOB).The pluton is composed principally of coarse monzonitic granite,fine monzonitic granite and syenogranite.Detailed petrologic,geochronological,geochemical and Sr-Nd isotopic studies are carried out on the granitic rocks from the Huoremudeke pluton.Zircons analysis from the sampleyields a weighted average mean 206Pb/238 U age of(222.3±1.8)Ma(MSWD=1.6),representing the intruding age of the pluton.Geochemically,the granitic rocks are characterized by high SiO_2,Al_2O_3,ALK,and low TiO_2,MnO,MgO and P_2O_5 contents,with fractionated REE patterns and negative Eu anomalies(δEu=0.37~0.50).They show enrichment of LILE,and depletion of HFSE on the primitive mantle-normalized trace element diagrams and have high Sr isotopic compositions(initial87Sr/86Sr=0.692 50~0.704 11)and weakly negativeεNd(t)values(-3.7~-2.7),with Nd model ages of 1.2~1.3Ga.It is considered that the granite is probably derived from dehydration melting of biotite-bearing pelite and its source area has residual plagioclase and ilmenite.Combined with the tectonic evolution of the Altay,it is proposed that the Huoremudeke granitic pluton is formed in the syn-collision environment.
【Fund】: 中国地质调查局地质调查项目(12120113071900);; 中央高校基本科研业务费资助项目(310827161002)
【CateGory Index】: P588.121
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【Citations】
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