GIG OpenIR  > 中科院广州地化所(-2008)  > 学位论文
扬子板块东南缘新元古代四堡期岩浆弧:来自浙北花岗质侵入体的年代学、地球化学和Nd-Hf-O同位素证据
叶美芳
Thesis Advisor李献华
Degree Grantor中国科学院广州地球化学研究所
Degree Name硕士
2007
Language中文
Document Type学位论文
Identifierhttp://ir.gig.ac.cn/handle/344008/3891
Collection中科院广州地化所(-2008)_学位论文
Recommended Citation
GB/T 7714
叶美芳. 扬子板块东南缘新元古代四堡期岩浆弧:来自浙北花岗质侵入体的年代学、地球化学和Nd-Hf-O同位素证据[D]. 中国科学院广州地球化学研究所,2007.
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