GYIG OpenIR  > 矿床地球化学国家重点实验室
滇西北休瓦促晚白垩世高分异 I 型花岗岩成因及其 对藏东地区晚中生代构造演化的限定
王新松;  胡瑞忠;  毕献武;  冷成彪;  潘力川;  朱经经;  陈佑玮
2015
Conference Name中国矿物岩石地球化学学会第15届学术年会
Conference Date2015-06-24
Conference Place中国吉林长春
Indexed ByCSCD
Language中文
Citation statistics
Document Type会议论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/9734
Collection矿床地球化学国家重点实验室
Affiliation1.中国科学院地球化学研究所/矿床地球化学国家重点实验室,贵阳 550002
2.中国科学院大学,北京 100049
Recommended Citation
GB/T 7714
王新松;胡瑞忠;毕献武;冷成彪;潘力川;朱经经;陈佑玮. 滇西北休瓦促晚白垩世高分异 I 型花岗岩成因及其 对藏东地区晚中生代构造演化的限定[C],2015.
Files in This Item:
File Name/Size DocType Version Access License
滇西北休瓦促晚白垩世高分异 I 型花岗岩(363KB)会议论文 开放获取CC BY-NC-SAView Application Full Text
Related Services
Recommend this item
Bookmark
Usage statistics
Export to Endnote
Google Scholar
Similar articles in Google Scholar
[王新松;胡瑞忠;毕献武;冷成彪;潘力川;朱经经;陈佑玮]'s Articles
Baidu academic
Similar articles in Baidu academic
[王新松;胡瑞忠;毕献武;冷成彪;潘力川;朱经经;陈佑玮]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[王新松;胡瑞忠;毕献武;冷成彪;潘力川;朱经经;陈佑玮]'s Articles
Terms of Use
No data!
Social Bookmark/Share
File name: 滇西北休瓦促晚白垩世高分异 I 型花岗岩成因及其.pdf
Format: Adobe PDF
All comments (0)
No comment.
 

Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.