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GIG OpenIR  > 中科院广州地化所(-2008)
张辉煌; 徐义刚; 葛文春; 马金龙
吉林伊通－大屯地区晚中生代－新生代玄武岩的地球化学特征及其意义
Source Publication岩石学报
ISSN1000-0569
2006
Volume22Issue:6Pages:1579-1596
Language中文
Indexed Bysci
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/13115
Collection中科院广州地化所(-2008)
Recommended Citation
GB/T 7714		 张辉煌,徐义刚,葛文春,等. 吉林伊通－大屯地区晚中生代－新生代玄武岩的地球化学特征及其意义[J]. 岩石学报,2006,22(6):1579-1596.
APA 张辉煌,徐义刚,葛文春,&马金龙.(2006).吉林伊通－大屯地区晚中生代－新生代玄武岩的地球化学特征及其意义.岩石学报,22(6),1579-1596.
MLA 张辉煌,et al."吉林伊通－大屯地区晚中生代－新生代玄武岩的地球化学特征及其意义".岩石学报 22.6(2006):1579-1596.
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