globalchange  > 影响、适应和脆弱性
DOI: 10.1007/s00531-015-1252-5
Scopus记录号: 2-s2.0-84945468911
论文题名:
From mantle roots to surface eruptions: Cenozoic and Mesozoic continental basaltic magmatism
作者: Kämpf H.; Németh K.; Puziewicz J.; Mrlina J.; Geissler W.H.
刊名: International Journal of Earth Sciences
ISSN: 14373254
出版年: 2015
卷: 104, 期:8
起始页码: 1909
结束页码: 1912
语种: 英语
英文摘要: [无可用摘要]
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84945468911&doi=10.1007%2fs00531-015-1252-5&partnerID=40&md5=4a86ff2b0160647dc0b12f677301c522
Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/70257
Appears in Collections:影响、适应和脆弱性
气候减缓与适应

Files in This Item:

There are no files associated with this item.


作者单位: German Research Centre for Geosciences GFZ Potsdam, Telegrafenberg, Potsdam, Germany; Volcanic Risk Solutions, Institute of Agriculture and Environment, Massey University, Private Bag 11 222, Palmerston North, New Zealand; Institute of Geological Sciences, University of Wrocław, Pl. M. Borna 9, 50-204, Wrocław, Poland; Institute of Geophysics, Czech Academy of Sciences, Bocni II/1401, Prague, Czech Republic; Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung, Am Alten Hafen 26, Bremerhaven, Germany

Recommended Citation:
Kämpf H.,Németh K.,Puziewicz J.,et al. From mantle roots to surface eruptions: Cenozoic and Mesozoic continental basaltic magmatism[J]. International Journal of Earth Sciences,2015-01-01,104(8)
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Kämpf H.]'s Articles
[Németh K.]'s Articles
[Puziewicz J.]'s Articles
百度学术
Similar articles in Baidu Scholar
[Kämpf H.]'s Articles
[Németh K.]'s Articles
[Puziewicz J.]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Kämpf H.]‘s Articles
[Németh K.]‘s Articles
[Puziewicz J.]‘s Articles
Related Copyright Policies
Null
收藏/分享
所有评论 (0)
暂无评论
 

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