globalchange  > 气候减缓与适应
DOI: 10.1002/grl.50746
论文题名:
Deep seismic reflection profile in Central Europe reveals complex pattern of Paleozoic and Alpine accretion at the East European Craton margin
作者: Malinowski M.; Guterch A.; Narkiewicz M.; Probulski J.; Maksym A.; Majdański M.; Środa P.; Czuba W.; Gaczyński E.; Grad M.; Janik T.; Jankowski L.; Adamczyk A.
刊名: Geophysical Research Letters
ISSN: 0094-8730
EISSN: 1944-8461
出版年: 2013
卷: 40, 期:15
起始页码: 3841
结束页码: 3846
语种: 英语
英文关键词: Baltica ; crustal structure ; Europe ; reflection seismics ; Teisseyre-Tornquist Zone
Scopus关键词: Baltica ; Crustal structure ; Deep seismic reflection profiles ; East-European craton ; Europe ; Reflection seismics ; Strike slip faulting ; Tectonic deformations ; Seismic waves ; Strike-slip faults ; Tectonics ; Geochronology ; accretion ; alpine environment ; collision zone ; crustal structure ; Paleozoic ; seismic reflection ; suture zone ; Central Europe ; East European Craton
英文摘要: The first deep reflection seismic profile was acquired across the Teisseyre-Tornquist Zone (TTZ), a major European suture zone, southeast of the Avalonia-Baltica collision zone, portraying different tectonic deformation styles (thick- versus thin-skinned) and Phanerozoic crustal accretion episodes over a relatively short distance (240 km). The overall crustal structure preserves image of the Neoproterozoic passive margin setting but with a significant overprint of the repetitive tectonic convergence (Cadomian to Alpine) acting at the Baltica margin. In contrast to the Avalonia-Baltica collision zone, here the polygenetic crustal accretion occurring at the cratonic margin was ultimately shaped by significant strike-slip faulting. TTZ is imaged as a narrow (10-15 km) transform zone separating the thinned East European cratonic crust from the Małopolska Block. © 2013. American Geophysical Union. All Rights Reserved.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84880905783&doi=10.1002%2fgrl.50746&partnerID=40&md5=730db366ebd7ceb03362a481a8f3a2d4
Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/5994
Appears in Collections: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 Geophysics, Polish Academy of Sciences, Ks. Janusza 64, 01-452 Warsaw, Poland

Recommended Citation:
Malinowski M.,Guterch A.,Narkiewicz M.,et al. Deep seismic reflection profile in Central Europe reveals complex pattern of Paleozoic and Alpine accretion at the East European Craton margin[J]. Geophysical Research Letters,2013-01-01,40(15).
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Malinowski M.]'s Articles
[Guterch A.]'s Articles
[Narkiewicz M.]'s Articles
百度学术
Similar articles in Baidu Scholar
[Malinowski M.]'s Articles
[Guterch A.]'s Articles
[Narkiewicz M.]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Malinowski M.]‘s Articles
[Guterch A.]‘s Articles
[Narkiewicz M.]‘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.