Zircon U-Pb ages and Hf isotope of the granitoids from the Xingwen porphyry molybdenum deposit in the Xiaoxing'an Range - Zhangguangcai Range metallogenic belt, NE China
Zeng, Qingdong1; Wang, Ruiliang2; Cheng, Guohua1; Yang, Yueheng1
刊名GEOLOGICAL JOURNAL
2018
卷号53期号:1页码:304-315
关键词U-pb Zircon Age Hf Isotope Porphyry Mo Deposit Xiaoxing'an Range - Zhangguangcai Range Metallogenic Belt Northeast China
ISSN号0072-1050
DOI10.1002/gj.2892
文献子类Article
英文摘要The newly discovered Xingwen porphyry Mo deposit is located in the most southern segment of the Xiaoxing'an Range-Zhangguangcai Range metallogenic belt (XZMB), NE China. The Mo deposit occurs with a granitic complex consisting of monzogranite, porphyritic granite and felsite porphyry. The Zircon U-Pb ages of monzogranite, porphyritic granite and felsite porphyry are 170.3 +/- 2.1, 168.5 +/- 2.5, and 166.7 +/- 1.6Ma, respectively. The inherited zircons from the monzogranite and porphyritic granite yield U-Pb ages of 239.8 +/- 5.8 and 249.4 +/- 6.2Ma, respectively. These ages reveal that the Mo mineralization in the most southern segment of the XZMB took place in the Middle Jurassic, and is consistent with the epoch of the largest Daheishan Mo district in the XZMB. In contrast, Triassic ages of the inherited zircons are consistent with the ages of the Triassic magmatic activities along the E-W trending tectono-magmatic belt in the northern margin of the North China Craton. The epsilon Hf(t) of the monzogranite, porphyritic granite and felsite porphyry change from -17.1 to +6.7 , -16.9 to +2.9, -5.94 to -0.90, respectively. The Hf isotopic compositions indicate that old crustal source, juvenile crustal source or depleted mantle contributed to their origin. When compared with the granite in Daheishan Mo district in XZMB, the epsilon Hf(t) probably indicates that the granitic complex in the margin of the Central Asia Orogenic Belt may have more old crustal materials than the granitic complex in the inner region of the Central Asia Orogenic Belt. Copyright (c) 2017 John Wiley & Sons, Ltd.
WOS关键词LU-HF ; JILIN PROVINCE ; TRACE-ELEMENT ; OROGENIC BELT ; GOLD DEPOSIT ; ORE GENESIS ; NORTH CHINA ; GEOCHRONOLOGY ; CONSTRAINTS ; SYSTEMATICS
WOS研究方向Geology
语种英语
出版者WILEY
WOS记录号WOS:000419785900016
资助机构National Natural Science Foundation of China(41390443) ; National Natural Science Foundation of China(41390443) ; Major State Basic Research Program of China(2013 CB429804) ; Major State Basic Research Program of China(2013 CB429804) ; National Natural Science Foundation of China(41390443) ; National Natural Science Foundation of China(41390443) ; Major State Basic Research Program of China(2013 CB429804) ; Major State Basic Research Program of China(2013 CB429804) ; National Natural Science Foundation of China(41390443) ; National Natural Science Foundation of China(41390443) ; Major State Basic Research Program of China(2013 CB429804) ; Major State Basic Research Program of China(2013 CB429804) ; National Natural Science Foundation of China(41390443) ; National Natural Science Foundation of China(41390443) ; Major State Basic Research Program of China(2013 CB429804) ; Major State Basic Research Program of China(2013 CB429804)
内容类型期刊论文
源URL[http://ir.iggcas.ac.cn/handle/132A11/82530]  
专题中国科学院地质与地球物理研究所
通讯作者Zeng, Qingdong
作者单位1.Chinese Acad Sci, Key Lab Mineral Resources, Inst Geol & Geophys, POB 9825, Beijing 100029, Peoples R China
2.China Univ Geosci, Sch Earth Sci & Resources, Beijing, Peoples R China
推荐引用方式
GB/T 7714
Zeng, Qingdong,Wang, Ruiliang,Cheng, Guohua,et al. Zircon U-Pb ages and Hf isotope of the granitoids from the Xingwen porphyry molybdenum deposit in the Xiaoxing'an Range - Zhangguangcai Range metallogenic belt, NE China[J]. GEOLOGICAL JOURNAL,2018,53(1):304-315.
APA Zeng, Qingdong,Wang, Ruiliang,Cheng, Guohua,&Yang, Yueheng.(2018).Zircon U-Pb ages and Hf isotope of the granitoids from the Xingwen porphyry molybdenum deposit in the Xiaoxing'an Range - Zhangguangcai Range metallogenic belt, NE China.GEOLOGICAL JOURNAL,53(1),304-315.
MLA Zeng, Qingdong,et al."Zircon U-Pb ages and Hf isotope of the granitoids from the Xingwen porphyry molybdenum deposit in the Xiaoxing'an Range - Zhangguangcai Range metallogenic belt, NE China".GEOLOGICAL JOURNAL 53.1(2018):304-315.
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