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| 浙江青田石平川钾长花岗岩特征及其成因探讨 | |
| 引用本文： | 叶泽富,鄢云飞,张彦杰,万方.浙江青田石平川钾长花岗岩特征及其成因探讨[J].资源调查与环境,2010,31(2):87-92. |
| 作者姓名： | 叶泽富 鄢云飞 张彦杰 万方 |
| 作者单位： | 1. 中国地质大学资源学院,武汉,430074;浙江省地质勘查局第十一地质大队,温州,325006 2. 中国地质大学资源学院,武汉,430074 3. 南京地质矿产研究所,南京,210016 4. 浙江省地质勘查局第十一地质大队,温州,325006 |
| 摘 要： | 青田县石平川钼矿床是浙江省现已发现的规模最大的钼矿床,多数人认为石平川钼矿床的形成与钾长花岗岩有密切关系.本文主要从岩相学、岩石地球化学、LA-ICPMS锆石U-Pb年代学等方面研究石平川钾长花岗岩,并探讨其成岩环境及成因.研究表明,石平川岩体属于高钾钙碱性、弱过铝质S型花岗岩,其形成于早白垩世晚期挤压环境,源岩物质主要是壳源,并有少部分幔源物质成分参与. |
| 关 键 词： | 石平川钾长花岗岩 钼矿床 地球化学 U-Pb锆石年龄 S型花岗岩 |
Characteristics and genesis of Shipingchuan potash-feldspar granite in Qintian county, Zhejiang Province |
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| YE Ze-fu,YAN Yun-fei,ZHANG Yan-jie,WAN Fang.Characteristics and genesis of Shipingchuan potash-feldspar granite in Qintian county, Zhejiang Province[J].Resources Survey & Environment,2010,31(2):87-92. | |
| Authors: | YE Ze-fu YAN Yun-fei ZHANG Yan-jie WAN Fang |
| Institution: | YE Ze-fu1,2,YAN Yun-fei1,ZHANG Yan-jie3,WAN Fang2(1.Resources Institute of China University of Geosciences,Wuhan,430074,China)(2.The 11th.Geological Team of Zhejiang Province,Wenzhou,325006,China)(3.Nanjing Institute of Geology and Mineral Resources,Nanjing,210016,China) |
| Abstract: | hipingchuan Mo-deposit in Qingtian county is a biggest molybdenum deposit in Zhejiang province at present,and most of researchers consider that the genesis of this deposit is closely related to the K-feldspar granite.This paper studies petrography,petrogeochemistry,LA-ICPM zircon U-Pb geochronology of the K-feldspar granite to approach its diagenetic environment and genesis.The study shows that the Shipingchuan K-feldspar granite belongs to high potassium calc-alkaline,weakly peraluminous S-type granite,whi... |
| Keywords: | Shipingchuan potash-feldspar granite molybdenum deposit petrogeochemistry U-Pb zircon ages S-type granite |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ | |