IGSNRR OpenIR
thetraceelementdistributionpatternsofediacaranearlycambrianblackshalesandtheoriginofseleniumintheguangningareawesternguangdongprovincesouthchina
Tian Xinglei1; Luo Kunli1; Zuza Andrew V2
2017
Source Publicationactageologicasinica
ISSN1000-9515
Volume91Issue:6Pages:1978
AbstractThe Ediacaran and early Cambrian black shales are widespread across the South China Craton (Yangtze and Cathaysia blocks). However, the trace element distribution patterns of the Ediacaran and early Cambrian black shales in the Cathaysia Block are still unclear. In this study, thirty-four black shale samples in the Lechangxia Group (Ediacaran) and thirteen black shale samples in the lower Bacun Group (early Cambrian) from Guangning area, western Guangdong Province, South China, were analyzed for major and trace elements concentrations. Compared to the upper continental crust, the Ediacaran black shales exhibit strongly enriched Se, Ga,and As with enrichment factor values (EF) higher than 10, significantly enriched Bi and Rb (10>EF>5), weakly enriched Mo, Ba,Cs, V, In, Be, T1,and Th (5>EF>2), normal U,Cr, Cd, Sc, Pb, Cu, and Li (2>EF>0.5),and depleted Ni,Zn, Sr, and Co. Early Cambrian black shales display strongly enriched Se, Ga, and As, significantly enriched Ba, Bi, and Rb, weakly enriched Mo, Cs, Cd, V,U, Be, In, and Tl, normal Sc, Th, Cr, Li, Cu, Ni, and Pb and depleted Co, Zn, and Sr. Moreover, Se is the most enriched trace element in the Ediacaran and early Cambrian black shales: concentrations vary from 0.25 to 30.09 ppm and 0.54 to 5.01 ppm, and averaging 4.84 and 1.72 ppm, with average EF values of 96.87 and 34.32, for the Ediacaran and early Cambrian shales respectively. The average concentration of Se in the Ediacaran black shales is 2.8 times higher than that of early Cambrian black shales. Se contents in the Ediacaran and early Cambrian black shales exhibit significant variation (P = 0.03). Provenance analysis showed that Se contents of both the Ediacaran and early Cambrian black shales were without detrital provenance and volcanoclastic sources,but of hydrothermal origin. The deep sources of Se and the presence of pyrite may explain the higher Se contents in the Ediacaran black shales. Similar with the Se-rich characteristics of the contemporaneous black shales in the south Qingling Mountain and Yangtze block,the Ediacaran and early Cambrian black shales in Guangning area, Cathaysia, are also enriched in Se, which may provide a clue for looking for the selenium-rich resources in western Guangdong Province.
Language英语
Document Type期刊论文
Identifierhttp://ir.igsnrr.ac.cn/handle/311030/128008
Collection中国科学院地理科学与资源研究所
Affiliation1.中国科学院地理科学与资源研究所
2.Nevada Bureau of Mines and Geology, University of Nevada
First Author Affilication中国科学院地理科学与资源研究所
Recommended Citation
GB/T 7714
Tian Xinglei,Luo Kunli,Zuza Andrew V. thetraceelementdistributionpatternsofediacaranearlycambrianblackshalesandtheoriginofseleniumintheguangningareawesternguangdongprovincesouthchina[J]. actageologicasinica,2017,91(6):1978.
APA Tian Xinglei,Luo Kunli,&Zuza Andrew V.(2017).thetraceelementdistributionpatternsofediacaranearlycambrianblackshalesandtheoriginofseleniumintheguangningareawesternguangdongprovincesouthchina.actageologicasinica,91(6),1978.
MLA Tian Xinglei,et al."thetraceelementdistributionpatternsofediacaranearlycambrianblackshalesandtheoriginofseleniumintheguangningareawesternguangdongprovincesouthchina".actageologicasinica 91.6(2017):1978.
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
[Tian Xinglei]'s Articles
[Luo Kunli]'s Articles
[Zuza Andrew V]'s Articles
Baidu academic
Similar articles in Baidu academic
[Tian Xinglei]'s Articles
[Luo Kunli]'s Articles
[Zuza Andrew V]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[Tian Xinglei]'s Articles
[Luo Kunli]'s Articles
[Zuza Andrew V]'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.