GYIG OpenIR  > 矿床地球化学国家重点实验室
金衢盆地燕山期基性脉岩元素地球化学及其成因
齐有强; 胡瑞忠; 刘燊; 冯彩霞; 田建吉; 王涛; 冯光英
2009
Source Publication矿物学报
IssueS1Pages:21-22
Keyword金衢盆地 基性脉岩 赣杭构造带 燕山期 晚中生代 成岩过程 成因 伸展作用 晚白垩世 元素地球化学
Indexed ByCSCD
Language中文
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Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/9980
Collection矿床地球化学国家重点实验室
Corresponding Author胡瑞忠
Affiliation1.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
2.中国科学院研究生院
Recommended Citation
GB/T 7714
齐有强,胡瑞忠,刘燊,等. 金衢盆地燕山期基性脉岩元素地球化学及其成因[J]. 矿物学报,2009(S1):21-22.
APA 齐有强.,胡瑞忠.,刘燊.,冯彩霞.,田建吉.,...&冯光英.(2009).金衢盆地燕山期基性脉岩元素地球化学及其成因.矿物学报(S1),21-22.
MLA 齐有强,et al."金衢盆地燕山期基性脉岩元素地球化学及其成因".矿物学报 .S1(2009):21-22.
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