NIGPAS OpenIR  > 中国科学院南京地质古生物研究所
藏北双湖地区才多茶卡一带构造混杂岩中发现晚泥盆世和晚二叠世放射虫硅质岩
朱同兴; 张启跃; 董瀚; 王玉净; 于远山; 冯心涛
2006
Source Publication地质通报
ISSN1671-2552
Volume25Issue:12Pages:1413-1418
Keyword放射虫硅质岩 晚泥盆世 晚二叠世 双湖地区 西藏北部
Document Type期刊论文
Identifierhttp://ir.nigpas.ac.cn/handle/332004/3755
Collection中国科学院南京地质古生物研究所
Recommended Citation
GB/T 7714
朱同兴,张启跃,董瀚,等. 藏北双湖地区才多茶卡一带构造混杂岩中发现晚泥盆世和晚二叠世放射虫硅质岩[J]. 地质通报,2006,25(12):1413-1418.
APA 朱同兴,张启跃,董瀚,王玉净,于远山,&冯心涛.(2006).藏北双湖地区才多茶卡一带构造混杂岩中发现晚泥盆世和晚二叠世放射虫硅质岩.地质通报,25(12),1413-1418.
MLA 朱同兴,et al."藏北双湖地区才多茶卡一带构造混杂岩中发现晚泥盆世和晚二叠世放射虫硅质岩".地质通报 25.12(2006):1413-1418.
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