中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Zircon SHRIMP U-Pb geochronology of the granitoid intrusions from Jinchanggouliang-Erdaogou gold orefieid and its significance.

文献类型:期刊论文

作者Miao, LC; Fan, WM; Zhai, MG; Qiu, YM; McNaughton, NJ; Groves, DI
刊名ACTA PETROLOGICA SINICA
出版日期2003
卷号19期号:1页码:71-80
关键词granitoid intrusion zircon SHRIMP geochronology Jinchanggouliang-Erdaogou
ISSN号1000-0569
文献子类Article
英文摘要The SHRIMP U-Pb dating results on zircons from granitoid intrusions in Jinchanggouliang- Erdaogou gold orefield suggest that this region experienced at least three phases of magmatism during Mesozoic, which are represented by the emplacements of the Xitaizi monogranite, the Loushan pyroxene-bearing quartz diorite, and the Xiduomiangou granodiorite as well as dioritic dike at 218 +/- 4 Ma ( Indosinian), 161 +/- 1 Ma ( early Yanshanian) and 126 +/- 1 Ma ( late Yanshanian), respectively. The geochemical characteristics of these intrusions indicate that they were related to orogenesis, formed at intracontinental extensional periods of late- or post-orogenesis. The age of 126 +/- 1 Ma of the pre- or syn-gold mineralization dioritic dike from Erdaogou mine district constrains the maximum age of the gold mineralization in the area, which, in combination with previous geochronology data, indicates that gold mineralization in the area took place at between 126similar to118 Ma. This shows that the gold deposits in the district are essentially coeval with those of other gold-concentrating provinces in North China Craton, such as Jiaodong, Xiaoqinling and Liaodong, and further confirms that the late Yanshanian is the most important and extensive period of gold mineralization in north China. In addition, the similarities of the late timing of gold mineralization with respect to the latest felsic magmatism in these major gold-concentrating areas are probably indicative of that gold mineralization is likely a latest stage product of orogeneses or regional tectono-magmatism.
WOS关键词JIAODONG-PENINSULA ; CHINA ; DEPOSITS ; SCALE
WOS研究方向Geology
语种英语
WOS记录号WOS:000181176400008
出版者SCIENCE CHINA PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/78729]  
专题中国科学院地质与地球物理研究所
通讯作者Miao, LC
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
2.Univ Western Australia, Key Ctr Strateg Mineral Deposits, Dept Geol & Geophys, Nedlands, WA 6907, Australia
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Miao, LC,Fan, WM,Zhai, MG,et al. Zircon SHRIMP U-Pb geochronology of the granitoid intrusions from Jinchanggouliang-Erdaogou gold orefieid and its significance.[J]. ACTA PETROLOGICA SINICA,2003,19(1):71-80.
APA Miao, LC,Fan, WM,Zhai, MG,Qiu, YM,McNaughton, NJ,&Groves, DI.(2003).Zircon SHRIMP U-Pb geochronology of the granitoid intrusions from Jinchanggouliang-Erdaogou gold orefieid and its significance..ACTA PETROLOGICA SINICA,19(1),71-80.
MLA Miao, LC,et al."Zircon SHRIMP U-Pb geochronology of the granitoid intrusions from Jinchanggouliang-Erdaogou gold orefieid and its significance.".ACTA PETROLOGICA SINICA 19.1(2003):71-80.

入库方式: OAI收割

来源:地质与地球物理研究所

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