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华中超高压变质带中榴辉岩的稀土元素地球化学
黄智龙; 刘丛强; 肖化云; 许成; 李文博
2000
Source Publication矿物学报
Volume20Issue:3Pages:250-256
metadata_24其它
Abstract根据REE含量及其分配模式,华中超高压变质带中榴辉岩可大体分为六种类型,即LREE富集型、LREE富集+Eu正异常型、LREE富集+Eu负异常型、REE平坦型、MREE(中稀土)富集型和HREE富集型,主要为LREE富集型和LREE富集+Eu正异常型,不同地区榴辉岩REE类型可进行对比,不同地区同REE类型榴辉岩的REE特征相似。原岩恢复结果表明榴辉岩的原岩主要为来源于相对富集地幔的大陆拉斑玄武岩。
Keyword超高压变质带
Subject Area中国典型特殊区带大规模成矿作用及其动力学
Funding Organization国家杰出青年基金项目(批准号:49625304)资助
Indexed ByCSCD
Language中文
CSCD IDCSCD:690527
Citation statistics
Cited Times:1[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/240
Collection矿床地球化学国家重点实验室_矿床地球化学国家重点实验室_期刊论文
Recommended Citation
GB/T 7714
黄智龙,刘丛强,肖化云,等. 华中超高压变质带中榴辉岩的稀土元素地球化学[J]. 矿物学报,2000,20(3):250-256.
APA 黄智龙,刘丛强,肖化云,许成,&李文博.(2000).华中超高压变质带中榴辉岩的稀土元素地球化学.矿物学报,20(3),250-256.
MLA 黄智龙,et al."华中超高压变质带中榴辉岩的稀土元素地球化学".矿物学报 20.3(2000):250-256.
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