|Table of Contents|

Uranium Mineralization of Luliangian and Yanshanian in Huayangchuan Area of Xiaoqinling, China: Implications from Geochronology of U-bearing Pegmatite(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2022年第02期
Page:
191-206
Research Field:
基础地质与矿床地质
Publishing date:

Info

Title:
Uranium Mineralization of Luliangian and Yanshanian in Huayangchuan Area of Xiaoqinling, China: Implications from Geochronology of U-bearing Pegmatite
Author(s):
LI Pu-tao123 GU Ping-yang12 LI Yong-jun3 HE Shi-ping12 WANG Shuang-shuang12 ZHUANG Yu-jun12 CHEN Rui-ming12
(1. Xi’an Center of Geological Survey, China Geological Survey, Xi’an 710054, Shaanxi, China; 2. Orogen Research Center of Geological Survey, China Geological Survey, Xi’an 710054, Shaanxi, China; 3. School of Earth Science and Resources, Chang’an University, Xi’an 710054, Shaanxi, China)
Keywords:
pegmatite uranium deposit zircon U-Pb age monazite Luliangian Yanshanian Xiaoqinling North China Craton
PACS:
P597; P619.14
DOI:
10.19814/j.jese.2021.12001
Abstract:
Huayangchuan uranium deposit in the west of Xiaoqinling intracontinental orogenic belt, the southern margin of North China Craton, is a polymetallic deposit, which is dominated by U and Nb, and associated with Pb and REE. The existing chronological data show that there are two stages of Indosinian and Yanshanian uranium mineralization in Huayangchuan area. In recent years, a large number of U-bearing pegmatites have been found in Huayangchuan mining area. The petrography, mineralogy and U-Pb chronology of zircon and monazite from U-bearing pegmatites located in Caopinggou of Huayangchuan area were carried out. Zircon U-Pb dating in U-bearing pegmatites is(1 922.5±6.0)Ma, and the mineral assemblage of U-bearing pegmatites shows that there is mineralization in diagenetic stage, indicating that Luliangian(2.0-1.8 Ga)uranium mineralization occurs in the process of basement splicing in the southern margin of North China Craton. The monazites in U-bearing pegmatites have high REE contents with obvious fractionation between LREE and HREE, and the chondrite-normalized REE pattern is characterized by a tilt to right with strong negative Eu anomaly, showing the characteristics of late hydrothermal crystallization genesis of highly differentiated magma. Monazite U-Pb age((141.9±1.8)Ma)indicates that there is a superimposed transformation mineralization of the existing U-rich geological body by Yanshanian granite magmatic hydrothermal process. Therefore, in addition to Indosinian uranium mineralization, there are at least Luliangian uranium pre-enrichment integration mineralization and Yanshanian superimposed transformation mineralization in Huayangchuan area.

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Last Update: 2022-04-30