敦化-密山断裂带的平移距离:来自松嫩-张广才岭-佳木斯-兴凯地块古生代-中生代岩浆作用的制约

GIG OpenIR

	王枫; 许文良; 葛文春; 杨浩; 裴福萍; 吴韦
	敦化-密山断裂带的平移距离:来自松嫩-张广才岭-佳木斯-兴凯地块古生代-中生代岩浆作用的制约
Source Publication	岩石学报
ISSN	1000-0569
	2016
Volume	32 Issue:4 Pages:1129-1140
Language	中文
Indexed By	SCI
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/33113
Collection	中国科学院广州地球化学研究所
Recommended Citation GB/T 7714	王枫,许文良,葛文春,等. 敦化-密山断裂带的平移距离:来自松嫩-张广才岭-佳木斯-兴凯地块古生代-中生代岩浆作用的制约[J]. 岩石学报,2016,32(4):1129-1140.
APA	王枫,许文良,葛文春,杨浩,裴福萍,&吴韦.(2016).敦化-密山断裂带的平移距离:来自松嫩-张广才岭-佳木斯-兴凯地块古生代-中生代岩浆作用的制约.岩石学报,32(4),1129-1140.
MLA	王枫,et al."敦化-密山断裂带的平移距离:来自松嫩-张广才岭-佳木斯-兴凯地块古生代-中生代岩浆作用的制约".岩石学报 32.4(2016):1129-1140.

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