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Zircon U-Pb and molybdenite Re-Os geochronology and Sr-Nd-Pb-Hf isotopic constraints on the genesis of the Xuejiping porphyry copper deposit in Zhongdian, Northwest Yunnan, China
Cheng-Biao Leng; Xing-Chun Zhang; Rui-Zhong Hu; Shou-Xu Wang; Hong Zhong; Wai-Quan Wangc, Xian-Wu Bi
2012
Source PublicationJournal of Asian Earth Sciences
Volume60Issue:1Pages:31-48
AbstractThe Xuejiping porphyry copper deposit is located in northwestern Yunnan Province, China. Tectonically, it lies in the southern part of the Triassic Yidun island arc. The copper mineralization is mainly hosted in quartz-dioritic and quartz-monzonitic porphyries which intruded into clastic-volcanic rocks of the Late Triassic Tumugou Formation. There are several alteration zones including potassic, strong silicific and phyllic, argillic, and propylitic alteration zones from inner to outer of the mineralized porphyry bodies.
The ages of ore-bearing quartz-monzonitic porphyry and its host andesite are obtained by using the zircon SIMS U-Pb dating method, with results of 218.3 +/- 1.6 Ma (MSWD = 0.31, N = 15) and 218.5 +/- 1.6 Ma (MSWD = 0.91, N = 16), respectively. Meanwhile, the molybdenite Re-Os dating yields a Re-Os isochronal age of 221.4 +/- 2.3 Ma (MSWD = 0.54, N = 5) and a weighted mean age of 219.9 +/- 0.7 Ma (MSWD = 0.88). They are quite in accordance with the zircon U-Pb ages within errors. Furthermore, all of them are contemporary with the timing of the Garze-Litang oceanic crust subduction in the Yidun arc. Therefore, the Xuejiping deposit could be formed in a continental margin setting.
There are negative epsilon(Nd)(t) values ranging from -3.8 to -2.1 and relatively high initial Sr-87/Sr-86 ratios from 0.7051 to 0.7059 for the Xuejiping porphyries and host andesites. The (Pb-206/Pb-204)(t), (Pb-207/Pb-204)(t) and (Pb-208/Pb-204)(t) values of the Xuejiping porphyries and host andesites vary from 17.899 to 18.654, from 15.529 to 15.626, and from 37.864 to 38.52, respectively, indicative of high radiogenic Pb isotopic features. In situ Hf isotopic analyses on zircons by using LA-MC-ICP-MS exhibit that there are quite uniform and slightly positive epsilon(Hf)(t) values ranging from -0.2 to +3.2 (mostly between 0 and +2), corresponding to relatively young single-stage Hf model ages from 735 Ma to 871 Ma. These isotopic features suggest that the primary magmas of the Xuejiping porphyries and their host andesites were mainly derived from a metasomatized mantle, with contamination of about 5-10% crustal rocks during ascending.
Comparing with typical porphyry Cu deposits, the Xuejiping porphyry Cu deposit is distinct by strong silicific and phyllic alteration and major stockwork veining mineralization in the ore-bearing porphyries, but lack of pervasive potassic alteration and disseminated mineralization. This indicates that there could be more prospective Cu resources in the Xuejiping ore district.
Indexed BySCI
Language英语
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/5122
Collection矿床地球化学国家重点实验室_矿床地球化学国家重点实验室_期刊论文
矿床地球化学国家重点实验室
Corresponding AuthorCheng-Biao Leng
Recommended Citation
GB/T 7714
Cheng-Biao Leng,Xing-Chun Zhang,Rui-Zhong Hu,et al. Zircon U-Pb and molybdenite Re-Os geochronology and Sr-Nd-Pb-Hf isotopic constraints on the genesis of the Xuejiping porphyry copper deposit in Zhongdian, Northwest Yunnan, China[J]. Journal of Asian Earth Sciences,2012,60(1):31-48.
APA Cheng-Biao Leng,Xing-Chun Zhang,Rui-Zhong Hu,Shou-Xu Wang,Hong Zhong,&Wai-Quan Wangc, Xian-Wu Bi.(2012).Zircon U-Pb and molybdenite Re-Os geochronology and Sr-Nd-Pb-Hf isotopic constraints on the genesis of the Xuejiping porphyry copper deposit in Zhongdian, Northwest Yunnan, China.Journal of Asian Earth Sciences,60(1),31-48.
MLA Cheng-Biao Leng,et al."Zircon U-Pb and molybdenite Re-Os geochronology and Sr-Nd-Pb-Hf isotopic constraints on the genesis of the Xuejiping porphyry copper deposit in Zhongdian, Northwest Yunnan, China".Journal of Asian Earth Sciences 60.1(2012):31-48.
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