岩矿测试

文章摘要

郑国栋,李建康,陈振宇,陈郑辉,侯可军,赵芝.赣南吉埠黄沙岩体的锆石铀-铅年代学研究及其地质意义[J].岩矿测试,2012,31(4):711-716

ZHENG Guo-dong,LI Jian-kang,CHEN Zhen-yu,CHEN Zheng-hui,HOU Ke-jun,ZHAO Zhi.U-Pb Dating of Zircon from Jibu Huangsha Intrusions in Southern Jiangxi Province and Its Geological Significances[J].Rock and Mineral Analysis,2012,31(4):711-716.DOI:

赣南吉埠黄沙岩体的锆石铀-铅年代学研究及其地质意义

HTML 下载全文 EndNote BibTeX 查看/发表评论下载PDF阅读器

U-Pb Dating of Zircon from Jibu Huangsha Intrusions in Southern Jiangxi Province and Its Geological Significances

投稿时间：2011-12-20

DOI：

中文关键词: 吉埠黄沙岩体 LA-MC-ICPMS U-Pb定年印支期稀土矿床

英文关键词: Jibu Huangsha granite LA-MC-ICPMS U-Pb dating Indo-Chinese epoch rare earth element deposit

基金项目:中国博士后科学基金和特别资助项目(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)

作者	单位	E-mail
郑国栋	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
李建康	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	Li9968@126.com
陈振宇	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
陈郑辉	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
侯可军	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
赵芝	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

摘要点击次数: 1431

全文下载次数: 1141

中文摘要:

赣南地区吉埠黄沙岩体的风化壳产出离子吸附型稀土矿床,但对其年代归属缺乏准确认识。利用从黄沙岩体风化壳中挑选出的锆石,开展了U-Pb法年代学研究。激光剥蚀-多接收器电感耦合等离子体质谱法(LA-MC-ICPMS)分析表明,岩体的²⁰⁶Pb/²³⁸U加权平均年龄为(242.5±1.8)Ma,说明吉埠黄沙岩体的成岩时代为印支期初期,而不是前任推断的燕山期。结合南岭区域发现的其他印支期岩体可知,印支运动在华南地区具有广泛影响,岩浆活动规模和出露面积较以往认识增大。纬度较高的黄沙岩体发生稀土矿化的事实进一步说明,1∶20万兴国幅、井冈山幅,乃至宁化幅内的印支期岩体也具有发生稀土矿化的条件,在今后的找矿工作中应给予重视。

英文摘要:

Jibu Huangsha granitic intrusions in Southern Jiangxi province hosted several ion adsorption type rare earth element (REE) deposits, but it's diagenic age is still unknown. In this paper, the U-Pb age of zircon separated from the weathering crust of Jibu Huangsha granitic intrusions was dated by using Laser Ablation-Multicollector Inductively Coupled Plasma-Mass Spectrometry (LA-MC-ICPMS). The dating results show that the weighted average ²⁰⁶Pb/²³⁸U age is (242.5±1.8) Ma, which indicates that the Jibu Huangsha intrusion formed in the early Indo-Chinese epoch, instead of the Yanshan epoch as suggested in the geological report of the Xingguo unit in a scale of 1/200000. Combining with the reports of other Indosinian granites in the Nanling district, it was concluded that Indo-China movement had a great effect in the Nanling district and produced larger scale magmatic activity with more outcrop areas than was previously understood. The higher latitude of Huagnsha intrusion further indicated the intrusions described in the geological report of Xingguo, Jinggangshan, and even the Ninghua unit in a scale of 1/200000 also have the potential to host ion adsorption type REE deposits, which should be significant for ore prospecting.

主管单位：	中国科学技术协会
主办单位：	中国地质学会岩矿测试技术专业委员会国家地质实验测试中心