期刊文献+

Geochemical characteristics of REE in the Late Neo-proterozoic limestone from northern Anhui Province, China

Geochemical characteristics of REE in the Late Neo-proterozoic limestone from northern Anhui Province, China
下载PDF
导出
摘要 Ten representative limestone samples [six from Wangshan Formation(WL) and the other four from Gouhou Formation(GL)] were collected from outcrops of the northern Anhui Province, and REE concentrations in limestone were measured by ICP-MS. The depositional environment and source of the REE were analyzed, and the results implys that the total REE of samples are low compared with the recent marine sediments, which range from 9.61 to 54.18 mg/kg and an average of 22.93 mg/kg. The PAAS-normalized REE+Y patterns of limestone are characterized by(1) light REE depletion in WL and enrichment in GL with the values of(Nd/Yb)SN ranging form 0.65 to 0.91 and 1.12 to 1.46, respectively;(2) light negative Ce anomaly(0.85–1.02) and positive La anomaly(0.92–1.27); and(3) both Eu(0.91–1.23) and Y(1.42–2.38) expressing light positive anomaly. The character indicated that the depositional environment was oxygenated, with infection by the hydrothermal activity and contamination of detritus. Ten representative limestone samples [six from Wangshan Formation (WL) and the other four from Gou- hou Formation (GL)] were collected from outcrops of the northern Anhui Province, and REE concentrations in lime- stone were measured by ICP-MS. The depositional environment and source of the REE were analyzed, and the re- sults implys that the total REE of samples are low compared with the recent marine sediments, which range from 9.61 to 54.18 mg/kg and an average of 22.93 mg/kg. The PAAS-normalized REE+Y patterns of limestone are char- acterized by (1) light REE depletion in WL and enrichment in GL with the values of (Nd/Yb)sN ranging form 0.65 to 0.91 and 1.12 to 1.46, respectively; (2) light negative Ce anomaly (0.85-1.02) and positive La anomaly (0.92-1.27); and (3) both Eu (0.91-1.23) and Y (1.42-2.38) expressing light positive anomaly. The character indicated that the depositional environment was oxygenated, with infection by the hydrothermal activity and contamination of detritus.
出处 《Chinese Journal Of Geochemistry》 EI CAS CSCD 2014年第2期187-193,共7页 中国地球化学学报
基金 supported by the National Nature Science Foundation of China(Nos.41173106 and 41373095) the Natural Science Foundation of Anhui Province Education Department(Nos.KJ2013B289 and KJ2013A249) the Program for Innovative Research Team in Suzhou University(No.2013kjtd01)
关键词 稀土元素 灰岩样品 地球化学特征 安徽省 晚新元古代 中国 ICP-MS Ce异常 rare-earth elements geochemistry Late Neo-proterozoic limestone Anhui Province
  • 相关文献

参考文献4

二级参考文献51

共引文献633

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部