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峨眉山二滩高钛玄武岩Zr/Hf分异的指示意义
Implications of Zr/Hf Fractionation in the Ertan High-Ti Basalt

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严再飞 1   程礼军 2   王宏图 3   陈觅 1   周家喜 1  
文摘 对峨眉山二滩高钛玄武岩高场强元素的研究表明, Zr/Hf比值出现了明显分异, 可分为高Zr/Hf组和低 Zr/Hf组两组玄武岩. Zr/Hf比值的分异与岩浆结晶分异作用无关, 而是由部分熔融和地幔源区的不同所导致, 暗示高Zr/Hf组和低Zr/Hf组玄武岩分别具有不同的部分熔融条件和不同的地幔物质组分
其他语种文摘 Variations of high-field strength element(HFSE)of the Ertan high-Ti basalts in the Emeishan suggest that Zr/Hf ratios were fractionated. According to the fractionation, the Ertan high-Ti basalts can be devided into high Zr/Hf group and low Zr/Hf group based on Zr/Hf ratios. The fractionation of Zr/Hf is not related with crystallization of basaltic magmas but partial melting and distinct compositions of mantle. This implies that high Zr/Hf basalt and low Zr/Hf basalt possessed distinct compositions of mantle and underwent different surroundings of partial melting, respectively
来源 矿物学报 ,2011,31(1):36-42 【核心库】
关键词 高钛玄武岩 ; 高场强元素 ; 部分熔融 ; 不均一性
地址

1. 中国科学院地球化学研究所, 矿床地球化学国家重点实验室, 贵州, 贵阳, 550002  

2. 重庆地质矿产研究院, 重庆, 400042  

3. 重庆大学资源与环境学院, 重庆, 400030

语种 中文
文献类型 研究性论文
ISSN 1000-4734
学科 地质学
基金 贵州省项目
文献收藏号 CSCD:4173020

参考文献 共 57 共3页

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引证文献 2

1 王超 延边开山屯花岗闪长岩-石英闪长岩体年代学、地球化学特征及对古太平洋板块俯冲作用时限的制约 岩石学报,2016,32(9):2856-2866
被引 1

2 周芳春 湖南仁里铌钽矿床矿体地球化学特征及其成因意义 地质学报,2019,93(6):1392-1404
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