Author:
Su Bin,Chen Yi,Guo Shun,Liu Jingbo
Funder
National Basic Research Program of China
Chinese Academy of Sciences
National Science Foundation of China
Reference169 articles.
1. P–T path for ultrahigh-pressure garnet ultramafic rocks of the Cuaba Gneiss, Rio San Juan complex, Dominican Republic;Abbott;International Geology Review,2006
2. The dunitic mantle–crust transition zone in the Oman ophiolite: residue of melt–rock interaction, cumulates from high-MgO melts, or both?;Abily;Geology,2013
3. Geochemistry of Fe-rich peridotites and associated pyroxenites from Horní Bory, Bohemian Massif: insights into subduction-related melt–rock reactions;Ackerman;Chemical Geology,2009
4. Highly siderophile element geochemistry of peridotites and pyroxenites from Horni Bory, Bohemian Massif: implications for HSE behaviour in subduction-related upper mantle;Ackerman;Geochimica et Cosmochimica Acta,2013
5. Non-chondritic distribution of the highly siderophile elements in mantle sulphides;Alard;Nature,2000
Cited by
36 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献