| 江西赣县韩坊岩体的成岩时代及成矿条件分析 |
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| 引用本文： | 李建康,陈振宇,陈郑辉,侯可军,赵正.江西赣县韩坊岩体的成岩时代及成矿条件分析[J].岩矿测试,2012,31(4):717-723. |
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| 作者姓名： | 李建康 陈振宇 陈郑辉 侯可军 赵正 |
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| 作者单位： | 1. 国土资源部成矿作用与资源评价重点实验室,中国地质科学院矿产资源研究所,北京100037;长安大学地球科学与资源学院,陕西西安710054
2. 国土资源部成矿作用与资源评价重点实验室,中国地质科学院矿产资源研究所,北京100037 |
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| 基金项目： | 中国博士后科学基金和特别资助(2008044018,200902580); 中国地质大调查项目(1212011120989,1212010633903); 国家深部探测技术与实验研究专项(SinoProbe 0301, SinoProbe0303); 中央级公益性科研院所基本科研业务费专项资金(K1001) |
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| 摘 要： | 选择我国重要的离子吸附型稀土矿床产地———韩坊花岗岩体开展了锆石激光剥蚀-多接收器电感耦合等离子体质谱法(LA-MC-ICPMS)定年工作。研究结果表明,岩体中锆石的晶型较完整,环带明显,属于典型的岩浆锆石;韩坊岩体存在两期岩浆活动,粗粒黑云二长花岗岩形成于加里东期,而细粒黑云二长花岗岩形成于燕山早期。加里东期的花岗岩是扬子陆块与华夏陆块拼接的结果,燕山期花岗岩是古太平洋板块向华南板块俯冲而导致岩石圈拆沉和减薄的结果。如果说南岭燕山期花岗岩控制了大规模钨锡成矿作用的发生,则加里东期花岗岩对南岭离子吸附型稀土矿床的形成具有重要贡献。加里东期的花岗岩含有褐帘石、锆石、萤石等易风化的富稀土副矿物,且因经受多起构造事件,断裂发育,加之多位于炎热多雨的地理位置,易于遭受强烈的风化作用。因此,易于形成离子吸附型稀土矿床。
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| 关 键 词： | 韩坊岩体 LA-MC-ICPMSU-Pb定年 加里东期 离子吸附型稀土矿床 |
| 收稿时间： | 2011/12/20 0:00:00 |
The Dating and Analysis of Ore-forming Conditions for Hanfang Granite Intrusions in Ganxian, Jiangxi Province |
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| LI Jian-kang,CHEN Zhen-yu,CHEN Zheng-hui,HOU Ke-jun and ZHAO Zheng.The Dating and Analysis of Ore-forming Conditions for Hanfang Granite Intrusions in Ganxian, Jiangxi Province[J].Rock and Mineral Analysis,2012,31(4):717-723. |
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| Authors: | LI Jian-kang CHEN Zhen-yu CHEN Zheng-hui HOU Ke-jun and ZHAO Zheng |
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| Institution: | Key Laboratory of Metallogeny and Mineral Resource Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China;College of Earth Science and Resources, Chang'an University, Xi'an 710054, China;Key Laboratory of Metallogeny and Mineral Resource Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China;Key Laboratory of Metallogeny and Mineral Resource Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China;Key Laboratory of Metallogeny and Mineral Resource Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China;Key Laboratory of Metallogeny and Mineral Resource Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China |
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| Abstract: | Zircons collected from Hanfang intrusions in Ganxian, Jiangxi province, whose weathered crust produced many rare earth element (REE) deposits, have been dated by using Laser Ablation-Multicollector Inductively Coupled Plasma-Mass Spectrometry (LA-MC-ICPMS) and are presented here. The dating results from typical magmatic zircons with good shape and oscillatory zoning show that the coarse-grained biotite monzonitic granite intruded in the Caledonian era, during the convergence between Yangtse block and Cathaysia block, and the fine-grained biotite monzonitic granite intruded in the early Yanshan epoch as the results of lithospheric thinning and delamination during subduction of the old Pacific plate to the South China Plate. The granite intrusions formed in the Yanshan epoch have a close relationship with large scale mineralization of W, Sn in the Nanling district, while the intrusions formed in the Caledonian era have a significant contribution to the formation of ion adsorption type REE deposits. The intrusions in the Caledonian era host REE-rich accessory minerals, such as orthite, zircon and fluorite. The fractures of the intrusions were well developed as a result of a few tectonic events. The bad weathering was attributed to the hot and rainy climate in this region. Therefore, the intrusions in the Caledonian era tend to produce ion adsorption type REE deposits for the reasons previously mentioned. |
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| Keywords: | Hanfang granite intrusion LA-MC-ICPMS U-Pb dating Caledonian ion adsorption type REE deposit |
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