Geochemistry of REY-Enriched Phosphorites in Zhijin Region, Guizhou Province, SW China: Insight into the Origin of REY

The rare earth elements and yttrium (REY)-enriched phosphorites in the Zhijin region, southwest China, have attracted much attention, yet its origin has not been sufficiently addressed. The geology, mineralogy and geochemistry of samples from four sections of the early Cambrian age from the Zhijin r...

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Main Authors: Shan He, Yong Xia, Jiafei Xiao, Daniel Gregory, Zhuojun Xie, Qinping Tan, Haiying Yang, Haiyan Guo, Shengwei Wu, Xingxiang Gong
Format: Article
Language:English
Published: MDPI AG 2022-03-01
Series:Minerals
Subjects:
Online Access:https://www.mdpi.com/2075-163X/12/4/408
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author Shan He
Yong Xia
Jiafei Xiao
Daniel Gregory
Zhuojun Xie
Qinping Tan
Haiying Yang
Haiyan Guo
Shengwei Wu
Xingxiang Gong
author_facet Shan He
Yong Xia
Jiafei Xiao
Daniel Gregory
Zhuojun Xie
Qinping Tan
Haiying Yang
Haiyan Guo
Shengwei Wu
Xingxiang Gong
author_sort Shan He
collection DOAJ
description The rare earth elements and yttrium (REY)-enriched phosphorites in the Zhijin region, southwest China, have attracted much attention, yet its origin has not been sufficiently addressed. The geology, mineralogy and geochemistry of samples from four sections of the early Cambrian age from the Zhijin region were studied to attain the redox condition and origin of REY. Data from in situ analysis show that REY are mainly contained in francolite, and the two types of francolite (bioclastic and granular) have no distinct difference in REY content (ΣREY). A Ce anomaly indicates an oxic condition in primary seawater. An Eu anomaly and ratios of redox sensitive elements (RSEs) indicate a fluctuating redox condition during phosphorite deposition. Shale-normalized REY patterns of whole rock and francolite show a hat-shaped pattern, indicating the effect of diagenetic processes. The Y/Ho ratio of the selected sections ranges from 38.13 to 61.93, and together with the Y anomaly, La<sub>N</sub>/Nd<sub>N</sub> ratio, La<sub>N</sub>/Sm<sub>N</sub> ratio, and La<sub>N</sub>/Yb<sub>N</sub> ratio, this indicates a seawater origin. This is supported by the Ce/Ce* of the phosphorite that ranges from 0.32 to 0.52 and the Eu/Eu* that ranges from 0.88 to 1.82, which is similar to the characteristics of seawater and deep-sea mud. We also propose a minor contribution of terrigenous debris and influence of diagenesis and hydrothermal processes.
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spelling doaj.art-a69abb06e06e4cfb8db0600a3d0dffc22023-12-03T13:45:32ZengMDPI AGMinerals2075-163X2022-03-0112440810.3390/min12040408Geochemistry of REY-Enriched Phosphorites in Zhijin Region, Guizhou Province, SW China: Insight into the Origin of REYShan He0Yong Xia1Jiafei Xiao2Daniel Gregory3Zhuojun Xie4Qinping Tan5Haiying Yang6Haiyan Guo7Shengwei Wu8Xingxiang Gong9State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, ChinaState Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, ChinaState Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, ChinaDepartment of Earth Sciences, University of Toronto, Earth Sciences Centre, 22 Ursula Franklin Street, Toronto, ON M5S 3B1, CanadaState Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, ChinaState Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, ChinaState Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, ChinaState Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, ChinaState Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, ChinaState Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, ChinaThe rare earth elements and yttrium (REY)-enriched phosphorites in the Zhijin region, southwest China, have attracted much attention, yet its origin has not been sufficiently addressed. The geology, mineralogy and geochemistry of samples from four sections of the early Cambrian age from the Zhijin region were studied to attain the redox condition and origin of REY. Data from in situ analysis show that REY are mainly contained in francolite, and the two types of francolite (bioclastic and granular) have no distinct difference in REY content (ΣREY). A Ce anomaly indicates an oxic condition in primary seawater. An Eu anomaly and ratios of redox sensitive elements (RSEs) indicate a fluctuating redox condition during phosphorite deposition. Shale-normalized REY patterns of whole rock and francolite show a hat-shaped pattern, indicating the effect of diagenetic processes. The Y/Ho ratio of the selected sections ranges from 38.13 to 61.93, and together with the Y anomaly, La<sub>N</sub>/Nd<sub>N</sub> ratio, La<sub>N</sub>/Sm<sub>N</sub> ratio, and La<sub>N</sub>/Yb<sub>N</sub> ratio, this indicates a seawater origin. This is supported by the Ce/Ce* of the phosphorite that ranges from 0.32 to 0.52 and the Eu/Eu* that ranges from 0.88 to 1.82, which is similar to the characteristics of seawater and deep-sea mud. We also propose a minor contribution of terrigenous debris and influence of diagenesis and hydrothermal processes.https://www.mdpi.com/2075-163X/12/4/408rare earth elements and yttriumphosphoritesfrancoliteGezhongwu formationorigin
spellingShingle Shan He
Yong Xia
Jiafei Xiao
Daniel Gregory
Zhuojun Xie
Qinping Tan
Haiying Yang
Haiyan Guo
Shengwei Wu
Xingxiang Gong
Geochemistry of REY-Enriched Phosphorites in Zhijin Region, Guizhou Province, SW China: Insight into the Origin of REY
Minerals
rare earth elements and yttrium
phosphorites
francolite
Gezhongwu formation
origin
title Geochemistry of REY-Enriched Phosphorites in Zhijin Region, Guizhou Province, SW China: Insight into the Origin of REY
title_full Geochemistry of REY-Enriched Phosphorites in Zhijin Region, Guizhou Province, SW China: Insight into the Origin of REY
title_fullStr Geochemistry of REY-Enriched Phosphorites in Zhijin Region, Guizhou Province, SW China: Insight into the Origin of REY
title_full_unstemmed Geochemistry of REY-Enriched Phosphorites in Zhijin Region, Guizhou Province, SW China: Insight into the Origin of REY
title_short Geochemistry of REY-Enriched Phosphorites in Zhijin Region, Guizhou Province, SW China: Insight into the Origin of REY
title_sort geochemistry of rey enriched phosphorites in zhijin region guizhou province sw china insight into the origin of rey
topic rare earth elements and yttrium
phosphorites
francolite
Gezhongwu formation
origin
url https://www.mdpi.com/2075-163X/12/4/408
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