GIG OpenIR  > 中科院广州地化所(-2008)
Geochemistry of the Middle Oligocene-Pliocene sandstones from the Nanpu Sag, the Bohai Bay Basin (Eastern China): Implications for provenance, weathering, and tectonic setting
Liu S
Source Publication12th International Symposium on Water-Rock Interaction (WRI-12)
2007-07-31
Conference Date2007-7-31
Conference PlaceKunming, PEOPLES R CHINA
Indexed BySCI
Language英语
AbstractMajor, trace and rare earth elements of 37 sandstones of the Middle Oligocene-Pliocene from the Nanpu Sag, Bohai Bay Basin were analyzed to evaluate their provenance, weathering, tectonic setting. Low-intermediate values of the Chemical Index of Alteration (CIA) reveal that these sandstones experienced relatively weak chemical weathering. Trace element ratios and REE characteristics show that the source rocks mainly consisted of felsic magmatic rocks that formed in the Yanshan Fold Belt during Mesozoic Yanshanian period. Tectonic setting discrimination diagrams show that the sandstones were deposited in a reactivated inner-continental setting, supporting the origin of the Bohai Bay Basin as being related to subduction of the Pacific plate towards the Eurasian plate.
Document Type会议论文
Identifierhttp://ir.gig.ac.cn/handle/344008/9428
Collection中科院广州地化所(-2008)
Recommended Citation
GB/T 7714
Liu S. Geochemistry of the Middle Oligocene-Pliocene sandstones from the Nanpu Sag, the Bohai Bay Basin (Eastern China): Implications for provenance, weathering, and tectonic setting[C],2007.
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
[Liu S]'s Articles
Baidu academic
Similar articles in Baidu academic
[Liu S]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[Liu S]'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.