[an error occurred while processing this directive] Global Geology 2018, 21(2) 91-107 DOI:   10.3969/j.issn.1673-9736.2018.02.02  ISSN: 1673-9736 CN: 22-1371/P
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zircon U-Pb geochronology
zircon Hf isotope
Late Triassic
granodiorite
petrogenesis
Wulonggou area
Eastern Kunlun orogen
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PubMed
Zircon U-Pb geochronology and Hf isotopic constraints on petrogenesis of Carnian Huanglonggou granodiorites inWulonggou area of Eastern Kunlun Orogen, NW China
SONG Kai, DING Qingfeng, ZHANG Qiang
College of Earth Sciences, Jilin University, Changchun 130061, China
ժҪ�� The Wulonggou area located in the Eastern Kunlun Orogen in NW China is characterized by extensive 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 granodiorite sample yielded a weighted mean U-Pb zircon age of ~221 Ma (Carnian).The Carnian granodiorite is metaluminous,with high alkalis contents of 6.37%-8.86%,high Al2O3 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 zircon εHf(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.
�ؼ����� zircon U-Pb geochronology   zircon Hf isotope   Late Triassic   granodiorite   petrogenesis   Wulonggou area   Eastern Kunlun orogen  
Zircon U-Pb geochronology and Hf isotopic constraints on petrogenesis of Carnian Huanglonggou granodiorites inWulonggou area of Eastern Kunlun Orogen, NW China
SONG Kai, DING Qingfeng, ZHANG Qiang
College of Earth Sciences, Jilin University, Changchun 130061, China
Abstract: The Wulonggou area located in the Eastern Kunlun Orogen in NW China is characterized by extensive 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 granodiorite sample yielded a weighted mean U-Pb zircon age of ~221 Ma (Carnian).The Carnian granodiorite is metaluminous,with high alkalis contents of 6.37%-8.86%,high Al2O3 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 zircon εHf(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.
Keywords: zircon U-Pb geochronology   zircon Hf isotope   Late Triassic   granodiorite   petrogenesis   Wulonggou area   Eastern Kunlun orogen  
�ո����� 2017-11-23 �޻����� 2017-12-20 ����淢������  
DOI: 10.3969/j.issn.1673-9736.2018.02.02
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Supported by Project of National Natural Science Foundation of China (No.41572056).

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