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

GIG OpenIR > 中科院广州地化所(-2008)

	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
Identifier	http://ir.gig.ac.cn/handle/344008/3891
Collection	中科院广州地化所(-2008)
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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