桂东南大容山－十万大山S型花岗岩带的成因：地球化学及Sr-Nd-Hf同位素制约

GIG OpenIR > 中科院广州地化所(-2008)

	祁昌实; 邓希光; 李武显; 李献华; 杨岳衡; 谢烈文
	桂东南大容山－十万大山S型花岗岩带的成因：地球化学及Sr-Nd-Hf同位素制约
Source Publication	岩石学报
ISSN	1000-0569
	2007
Volume	23 Issue:2 Pages:403-412
Language	中文
Indexed By	sci
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/13347
Collection	中科院广州地化所(-2008)
Recommended Citation GB/T 7714	祁昌实,邓希光,李武显,等. 桂东南大容山－十万大山S型花岗岩带的成因：地球化学及Sr-Nd-Hf同位素制约[J]. 岩石学报,2007,23(2):403-412.
APA	祁昌实,邓希光,李武显,李献华,杨岳衡,&谢烈文.(2007).桂东南大容山－十万大山S型花岗岩带的成因：地球化学及Sr-Nd-Hf同位素制约.岩石学报,23(2),403-412.
MLA	祁昌实,et al."桂东南大容山－十万大山S型花岗岩带的成因：地球化学及Sr-Nd-Hf同位素制约".岩石学报 23.2(2007):403-412.

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