globalchange  > 影响、适应和脆弱性
DOI: 10.1007/s00531-012-0841-9
Scopus记录号: 2-s2.0-84878106536
论文题名:
The Antarctic viewpoint of the Central Paratethys: Cause, timing, and duration of a deep valley incision in the Middle Miocene Alpine-Carpathian Foredeep of Lower Austria
作者: Gebhardt H.; Roetzel R.
刊名: International Journal of Earth Sciences
ISSN: 14373254
出版年: 2013
卷: 102, 期:4
起始页码: 977
结束页码: 987
语种: 英语
英文关键词: Alpine-Carpathian Foredeep ; Central Paratethys ; Glacio-eustatic sea-level changes ; Incised valley ; Middle Miocene
Scopus关键词: deposition ; erosion ; glacioeustacy ; incised valley ; marine sediment ; Miocene ; Paratethys ; sea level change ; Antarctica ; Austria ; Carpathian Foredeep ; Lower Austria ; Vienna Basin ; Paratethys
英文摘要: Global, glacio-eustatic sea-level changes massively influenced the depositional history of the Central Paratethyan region. Here, we correlate Middle Miocene global δ18O-shifts with ice volume changes on Antarctica and sea-level changes with corresponding phases of erosion (valley incision) and deposition in the Lower Austrian part of the Alpine-Carpathian Foredeep. This allows the exact dating of the valley formation. Two periods of positive δ18O-shifts resulted in sea-level drops of about 60 and 40 m, respectively. The first drop in the late Langhian (middle Badenian) at c. 13.9 Ma (Mi3b) was fast and caused severe erosion on the emerged foredeep. In a second, less pronounced step around 13.0 Ma (Mi4) in the middle Serravallian (late Badenian), the base level was further deepened after a period of alternating erosion and deposition. The combined sea-level change (80-120 m) fits well with the maximum thickness of Sarmatian sediments drilled within incised valley (110 m). The global sea-level falls affected not only the geological history of the foredeep. The intensive erosion (valley incision) is combined with delta progradation in the adjacent Vienna Basin. Due to this massive sea-level drop, the interruption of marine connections resulted in vast salt deposits and faunal crises within the Central Paratethys during this time. © 2012 Springer-Verlag Berlin Heidelberg.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84878106536&doi=10.1007%2fs00531-012-0841-9&partnerID=40&md5=1c606e6dd5d354610ebf1708cae4d57c
Citation statistics:
被引频次[WOS]:5   [查看WOS记录]     [查看WOS中相关记录]
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/70550
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: Geologische Bundesanstalt, Neulinggasse 38, 1030 Vienna, Austria

Recommended Citation:
Gebhardt H.,Roetzel R.. The Antarctic viewpoint of the Central Paratethys: Cause, timing, and duration of a deep valley incision in the Middle Miocene Alpine-Carpathian Foredeep of Lower Austria[J]. International Journal of Earth Sciences,2013-01-01,102(4)
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Gebhardt H.]'s Articles
[Roetzel R.]'s Articles
百度学术
Similar articles in Baidu Scholar
[Gebhardt H.]'s Articles
[Roetzel R.]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Gebhardt H.]‘s Articles
[Roetzel R.]‘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.