Zircon U-Pb geochronology and Hf isotopic constraints on petrogenesis of Carnian Huanglonggou granodiorites in Wulonggou area of Eastern Kunlun Orogen,NW China |
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Authors: | SONG Kai DING Qingfeng ZHANG Qiang |
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Abstract: | The Wulonggou area located in the Eastern Kunlun Orogen in NW China is characterized by exten-sive granitoid magmatism, ductile faulting and orogenic gold mineralization.The Huanglonggou granodiorite is cut by an orogenic gold-bearing fault.This study investigated the major and trace-element compositions, zircon U-Pb dates and zircon Hf isotopic compositions of the Huanglonggou granodiorite.One Huanglonggou granodior-ite sample yielded a weighted mean U-Pb zircon age of ~221 Ma ( Carnian) .The Carnian granodiorite is meta-luminous, with high alkalis contents of 6.37%-8.86%, high Al2 O3 contents of 15.41%-16.19%, high Sr contents of (426--475) ×10 -6 , relatively high Sr/Y ratios, high ( La/Yb) N values and low HREE, suggesting an adakite type high-SiO2 granite.The Huanglonggou granodiorite sample has zirconεHf ( t) values ranging from-4.4 to +1.1.These Hf isotopic data suggest that the Carnian granodiorite was likely derived from the partial melting of subducted Paleo-Tethys oceanic slab.It is suggested that the Late Triassic granodiorite was emplaced during the northward subduction of Paleo-Tethys oceanic slab.Orogenic gold mineralization in the Wulonggou area formed after the emplacement of the Late Triassic intrusive rocks. |
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