globalchange  > 影响、适应和脆弱性
DOI: 10.1007/s00531-014-1134-2
Scopus记录号: 2-s2.0-84945438118
论文题名:
Subcontinental lithospheric mantle beneath Central Europe
作者: Puziewicz J.; Matusiak-Małek M.; Ntaflos T.; Grégoire M.; Kukuła A.
刊名: International Journal of Earth Sciences
ISSN: 14373254
出版年: 2015
卷: 104, 期:8
起始页码: 1913
结束页码: 1924
语种: 英语
英文关键词: Central Europe ; Lithology ; Lithospheric mantle ; Metasomatism
Scopus关键词: clinopyroxene ; dissolution ; harzburgite ; Hercynian orogeny ; lithology ; lithospheric structure ; mantle structure ; melting ; metasomatism ; rifting ; Silesian ; xenolith ; Bohemian Massif ; Eger ; Germany ; Heves ; Hungary ; Lusatia
英文摘要: Mantle xenoliths in Oligocene–Miocene alkaline lavas in Lower Silesia (SW Poland) and adjacent part of Upper Lusatia (SE Germany) are samples of the subcontinental lithospheric mantle at the time of culmination of rifting in the Eger Rift (Bohemian Massif, Central Europe). The xenoliths come from the spinel mantle facies and show that two major lithologies occur in the area: A—highly magnesian (olivine Fo 90.5–92.0) harzburgites, and B—less magnesian (olivine Fo 84.0–90.0) harzburgites. The protolith of group A was clinopyroxene-free harzburgite being the residue after extensive melting. It was affected by chromatographic carbonatite/silicate melt metasomatism, with the carbonatite metasomatism only recorded in distal parts of the chromatographic systems. The B harzburgites were penetratively metasomatised by percolating alkaline silicate melts at the time of volcanism. That metasomatism was mostly anhydrous and typically cryptic; it lowered the Mg/(Mg + Fe) ratio of olivine and orthopyroxene in the peridotites subjected to melt percolation and led in places to dissolution of clinopyroxene. The mostly harzburgitic subcontinental mantle lithospheric domain beneath Lower Silesia and Upper Lusatia differs from the lherzolitic/harzburgitic ones located to W and SW beneath other parts of European Variscan orogen. © 2014, The Author(s).
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84945438118&doi=10.1007%2fs00531-014-1134-2&partnerID=40&md5=cfd30e7bab8c2f09f2eb01589017cc94
Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/70229
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: Institute of Geological Sciences, University of Wrocław, Pl. M. Borna 9, Wrocław, Poland; Department of Lithospheric Research, University of Vienna, Althanstrasse 4, Vienna, Austria; Geosciences Environment Toulouse, Midi-Pyrénées Observatory, CNRS-IRD-Toulouse University, 14 av. E. Belin, Toulouse, France

Recommended Citation:
Puziewicz J.,Matusiak-Małek M.,Ntaflos T.,et al. Subcontinental lithospheric mantle beneath Central Europe[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
[Puziewicz J.]'s Articles
[Matusiak-Małek M.]'s Articles
[Ntaflos T.]'s Articles
百度学术
Similar articles in Baidu Scholar
[Puziewicz J.]'s Articles
[Matusiak-Małek M.]'s Articles
[Ntaflos T.]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Puziewicz J.]‘s Articles
[Matusiak-Małek M.]‘s Articles
[Ntaflos T.]‘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.