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Timing of hydrothermal activity associated with the Douzhashan uranium-bearing granite and its significance for uranium mineralization in northeastern Guangxi, China
  • ISSN号:0371-5736
  • 期刊名称:《地质论评》
  • 时间:0
  • 分类:P619.140.2[天文地球—矿床学;天文地球—地质学] P532[天文地球—古生物学与地层学;天文地球—地质学]
  • 作者机构:[1]State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210093, China
  • 相关基金:supported by the National Natural Science Foundation of China(41072028,41230315 and 40702012);the National Basic Research Program of China(2012CB416704);the China Nuclear Geological Survey Basic Research Program(2011-2015);the Doctoral Fund of the Ministry of Education of China(20100091110048)
中文摘要:

在东北 Guangxi 的 Miaoershan 铀(U) 矿石地是在华南的重要花岗石相关的 U 存款之一并且是仔细与 Douzhashan 忍受 U 花岗石有关。Douzhashan 花岗石包含主要 U 富有的附件矿物质,包括独居石(UO2 = 0.981.75 wt%) 并且磷钇矿(UO2 = 1.486.14 wt%) 。231 ns 的主要独居石和磷钇矿收益化学药品年龄。在这研究,二中生代中间酸的恼人的岩石的 LA-ICP-MS 锆石地球年代学(包括 Shima 斑状的 granodiorite 和 Gaozi 石英闪长岩斑岩) 在 Ningzhen,区域系统地被调查。这些新 geochronological 数据证明在 Ningzhen 区域的中间酸的 magmatism 标明日期到近似在 109 和 101 妈之间。我们为 Cishantou skarn 的现在的新 40Ar-39Ar 金云母年龄熨抑制在 Ningzhen 区域预定 mineralisation 的沉积物。在 Cishantou skarn 沉积物的金云母产出 104 的 40Ar-39Ar 高原年龄

英文摘要:

The Miaoershan uranium (U) ore field in northeastern Guangxi is one of the important granite-related U deposits in south China and is closely related to the Douzhashan U-bearing granite. The Douzhashan granite contains primary U-rich accessory minerals, including monazite (UO2 = 0.98-1.75 wt%) and xenotime (UO2 = 1.48-6.14 wt%). Primary monazite and xenotime yield chemi- cal ages of 231±28 Ma and 230 ±38 Ma by electron microprobe analysis and U-Pb isotopic ages of 220±6 Ma and 211±7 Ma by laser ablation-inductively coupled-mass spectrometry respectively. These ages demonstrate that the Douzhashan granite formed during the period of Indosinian magmatic activity. Back scattered electron imaging shows that monazite and xenotime are com- monly altered to assemblages of low-U synchisite and apatite, which was associated with loss of U to hydrothermal fluids. U-Th-Pb analyses of secondary apatite yielded a chemical age of 136± 17 Ma, which corresponds to the timing of Creta-ceous-Tertiary crustal extension in south China. We suggest that the heat and CO2 required for mineralization was the result of Yanshanian crustal extension, and that this triggered the breakdown of U-rich accessory minerals in the Douzhashan U-bearing granite. Uranium remobilization from the Douzhashan granite provided materials for mineralization within the granite and/or surrounding country rocks. Therefore, a combination of Indosinian compression and Yanshanian extensional overprint produced the hydrothermal U deposits associated with the Douzhashan granite.

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期刊信息
  • 《地质论评》
  • 北大核心期刊(2011版)
  • 主管单位:中国科学技术协会
  • 主办单位:中国地质学会
  • 主编:杨文采
  • 地址:北京阜成门外百万庄路26号中国地质学会期刊处
  • 邮编:100037
  • 邮箱:georeview@cags.ac.cn
  • 电话:010-68999804
  • 国际标准刊号:ISSN:0371-5736
  • 国内统一刊号:ISSN:11-1952/P
  • 邮发代号:2-382
  • 获奖情况:
  • 中国期刊方阵“双效”期刊
  • 国内外数据库收录:
  • 美国化学文摘(网络版),美国地质文献预评数据库,日本日本科学技术振兴机构数据库,中国中国科技核心期刊,中国北大核心期刊(2004版),中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版),中国北大核心期刊(2000版)
  • 被引量:23413