GIG OpenIR  > 同位素地球化学国家重点实验室
常翱飞1,2; 丁兴1,2,3
热扩散驱动的元素分异和同位素分馏:一种不容忽视的硅酸盐成分分异机制
Source Publication岩石学报
ISSN1000-0569
2020
Volume36Issue:1Pages:99-112
Language中文
WOS IDWOS:000533247400011
Citation statistics
Cited Times:1[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/57075
Collection同位素地球化学国家重点实验室
Affiliation1.中国科学院广州地球化学研究所,同位素地球化学国家重点实验室,广州510640;
2.中国科学院大学,北京100049;
3.中国科学院青藏高原地球科学卓越创新中心,北京100101
Recommended Citation
GB/T 7714
常翱飞,丁兴. 热扩散驱动的元素分异和同位素分馏:一种不容忽视的硅酸盐成分分异机制[J]. 岩石学报,2020,36(1):99-112.
APA 常翱飞,&丁兴.(2020).热扩散驱动的元素分异和同位素分馏:一种不容忽视的硅酸盐成分分异机制.岩石学报,36(1),99-112.
MLA 常翱飞,et al."热扩散驱动的元素分异和同位素分馏:一种不容忽视的硅酸盐成分分异机制".岩石学报 36.1(2020):99-112.
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