IGSNRR OpenIR
雅鲁藏布大峡谷地质成因
丁林1; 季建清2; 张进江1; 钟大赉1; 杨逸畴3
1999
Source Publication地学前缘
ISSN1005-2321
Volume006Issue:004Pages:231
Abstract文中总结了雅鲁藏布大峡谷科学探险考察中获得投奔 石学和构造地质学认识与区域上已经取得的多学科成果,论述了牙鲁藏布大峡谷得以形成的根本原因是该地区深部存在着地幔上涌体,雅鲁藏布大峡谷和大另弯的形成是地幔上涌体作用于岩石圈和地表的效应。地幔上涌体的确认揭开了该地区的特有的生物学,气候特征等方面的奥秘,雅鲁藏布大峡谷及其周缘地区是大陆动力学研究,壳-幔动力学,地球系统中各圈层间耦合作用及大陆块体运动学研
Language英语
Document Type期刊论文
Identifierhttp://ir.igsnrr.ac.cn/handle/311030/95699
Collection中国科学院地理科学与资源研究所
Affiliation1.中国科学院地质与地球物理研究所
2.北京大学
3.中国科学院地理科学与资源研究所
Recommended Citation
GB/T 7714
丁林,季建清,张进江,等. 雅鲁藏布大峡谷地质成因[J]. 地学前缘,1999,006(004):231.
APA 丁林,季建清,张进江,钟大赉,&杨逸畴.(1999).雅鲁藏布大峡谷地质成因.地学前缘,006(004),231.
MLA 丁林,et al."雅鲁藏布大峡谷地质成因".地学前缘 006.004(1999):231.
Files in This Item:
There are no files associated with this item.
Related Services
Recommend this item
Bookmark
Usage statistics
Export to Endnote
Google Scholar
Similar articles in Google Scholar
[丁林]'s Articles
[季建清]'s Articles
[张进江]'s Articles
Baidu academic
Similar articles in Baidu academic
[丁林]'s Articles
[季建清]'s Articles
[张进江]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[丁林]'s Articles
[季建清]'s Articles
[张进江]'s Articles
Terms of Use
No data!
Social Bookmark/Share
All comments (0)
No comment.
 

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