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

	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
ISSN	1671-2552
Volume	25 Issue:12 Pages: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
Identifier	http://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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