Application of Electron Probe Microanalyzer to Study the Textures and Compositions of Alteration Coronas of Monazite from the Longhuashan Granite, Northern Guangdong Province

ZHANG Long; CHEN Zhenyu; WANG Fangyue; ZHOU Taofa

doi:10.15898/j.cnki.11-2131/td.202109070118

2022 Vol. 41, No. 2

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ZHANG Long, CHEN Zhenyu, WANG Fangyue, ZHOU Taofa. Application of Electron Probe Microanalyzer to Study the Textures and Compositions of Alteration Coronas of Monazite from the Longhuashan Granite, Northern Guangdong Province[J]. Rock and Mineral Analysis, 2022, 41(2): 174-184. doi: 10.15898/j.cnki.11-2131/td.202109070118

Citation:

ZHANG Long, CHEN Zhenyu, WANG Fangyue, ZHOU Taofa. Application of Electron Probe Microanalyzer to Study the Textures and Compositions of Alteration Coronas of Monazite from the Longhuashan Granite, Northern Guangdong Province[J]. Rock and Mineral Analysis, 2022, 41(2): 174-184. doi: 10.15898/j.cnki.11-2131/td.202109070118

Application of Electron Probe Microanalyzer to Study the Textures and Compositions of Alteration Coronas of Monazite from the Longhuashan Granite, Northern Guangdong Province

1.
Ore Deposit and Exploration Center, School of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009, China
2.
Anhui Province Engineering Research Center for Mineral Resources and Mine Environments, Hefei 230009, China
3.
Key Laboratory of Metallogeny and Mineral Assessment, Ministry of Natural Resources; Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China

Received Date: 07 September 2021

Revised Date: 30 October 2021

Accepted Date: 11 November 2021

Publish Date: 28 March 2022

Abstract

Abstract

BACKGROUND
Monazite is a common uranium-bearing accessory mineral in granite-related uranium deposits in South China. The Longhuashan pluton is an important U-bearing granite in the Zhuguangshan batholith, Northern Guangdong. Distinct alteration coronas of monazite were observed in the pluton. However, textures and compositions of alteration coronas of monazite and their implications for uranium mineralization are still poorly understood.
OBJECTIVES
To investigate the detailed textural and compositional evolution of monazite in granites during alteration, and to provide insights into uranium mobilization and enrichment in granite-related uranium deposits.
METHODS
Textures and chemical compositions of alteration coronas of monazite were investigated using electron probe microanalyzer (EPMA).
RESULTS
Alteration coronas of monazite in the Longhuashan granite consisted of newly formed apatite, allanite, epidote, and Th-rich phases. The monazite alteration coronas area was a concentric zone composed of monazite, apatite (including thorium-rich minerals), and monazite-epidote from the inside to the outside. Mass balance calculations showed that during the alteration of monazite, light rare earth (LREE), Y, Th, and U elements were remobilized and migrated, and the fluid brought in elements such as Ca, Fe, Al, and F to form alteration coronas composed of apatite, epidote, and thorium-rich minerals. The EPMA mapping showed that monazite alteration led to the remobilization of uranium, but the uranium was mainly enriched in the altered coronas. In this pluton, 3.7% U was located in monazite, and more than 80% U was hosted by uraninite.
CONCLUSIONS
Monazite only contributes limited uranium to regional uranium mineralization, and uraninite is the most important host for uranium in the Longhuashan granite.
- monazite /
- alteration coronas /
- electron probe microanalyzer /
- Longhuashan granite /
- northern Guangdong

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