北喜马拉雅淡色花岗岩中发现4N5高纯石英原料:苦堆含石榴子石二云花岗岩
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1.中国地质大学(武汉);2.中国地质调查局成都地质调查中心(西南地质科技创新中心);3.中国地质调查局成都地质调查中心(西南地质科技创新中心);4.新疆维吾尔自治区地质局阿勒泰地质大队

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TD985;P619.233

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国家重点基础研究发展计划(973计划)


Discovery of 4N5-grade High-Purity Quartz raw material in the North Himalayan leucogranite: The Kudui Garnet-Bearing Gneissic Two-Mica Granite
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1.China University of Geosciences;2.Chengdu Center of China Geological Survey (Southwest China Geological Science and Technology Innovation Center);3.Altay Geological Brigade of Xinjiang Uygur Autonomous Region Bureau of Geology;4.School of Earth Resources, China University of Geosciences (Wuhan)

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    摘要:

    高纯石英是新一代信息技术、高端装备制造等战略性新兴产业的关键基础材料。然而,我国高端高纯石英原料长期依赖进口,资源安全面临严峻挑战。北喜马拉雅造山带发育巨量高分异淡色花岗岩,其石英中晶格杂质含量相对较低,展现出成为新型高纯石英原料的巨大潜力。为评估该地区高纯石英的找矿前景,本文选取北喜马拉雅苦堆穹窿北侧的苦堆含石榴子石片麻状二云花岗岩体作为研究对象,综合运用偏光显微镜、ICP-OES等设备,并结合系统的矿物提纯实验,详细分析了岩石学特征、石英中包裹体特征、杂质元素的赋存状态及提纯效果。结果表明:苦堆岩体石英中包裹体含量较少,以次生流体包裹体为主,易于通过物理化学方法去除;经提纯工艺处理后,石英砂中SiO?含量达到99.9958%(4N5级),接近国际IOTA-STD高纯石英标准。主要杂质元素Al(27.50×10??~27.65×10??)、Ti(3.40×10??~3.45×10??)和Li(5.64×10??~5.66×10??)的含量显著偏低,这与岩浆的高分异演化过程密切相关。杂质元素赋存状态分析显示,提纯后样品中(Al3?+Fe3?+B3?)/(Na?+K?+Li?+P??)比值为1.08~1.09(略大于1),表明仍有及少量的杂质以流体包裹体或矿物包裹体等形式存在。若改进提纯技术,进一步去除流体包裹体或矿物包裹体中的Na、K、Li等碱金属杂质,品质将进一步提升至4N6级以上。研究认为,苦堆岩体石英原料品质优良、提纯潜力巨大,已达到中高端高纯石英的质量要求。这一发现证实了北喜马拉雅淡色花岗岩具备形成规模性高纯石英矿床的成矿潜力,该区域是寻找优质高纯石英资源的重要目标区。

    Abstract:

    High-purity quartz is a key fundamental material for strategic emerging industries such as next-generation information technology and high-end equipment manufacturing. However, China''s high-end high-purity quartz raw materials have long been imported, posing severe challenges to resource security. Extensive highly fractionated leucogranites are hosted in the Northern Himalayan orogenic belt, and their quartz is characterized by relatively low lattice impurity content, which is shown to have great potential as a new type of high-purity quartz raw material. To evaluate the prospecting potential of high-purity quartz in this region, the Kudui garnet-bearing gneissic two-mica granite pluton on the northern side of the Kudui Dome in the Northern Himalayas was selected as the research object. Detailed analyses of petrological characteristics, inclusion features in quartz, occurrence states of impurity elements, and purification effects were conducted using polarizing microscopy, ICP-OES, and systematic mineral purification experiments. It is shown by the results that quartz in the Kudui pluton contains relatively few inclusions, mainly secondary fluid inclusions, which are easily removable by physico-chemical methods. After the purification process, the SiO? content in the quartz sand is determined to be 99.9958% (4N5 grade), approaching the international IOTA-STD high-purity quartz standard. The contents of major impurity elements, including Al (27.50×10??–27.65×10??), Ti (3.40×10??–3.45×10??), and Li (5.64×10??–5.66×10??), are found to be significantly low, which is closely related to the highly fractionated evolution of the magma. It is shown by analysis of impurity element occurrence states that the (Al3?+Fe3?+B3?)/(Na?+K?+Li?+P??) ratio in the purified samples is 1.08–1.09 (slightly greater than 1), indicating that trace amounts of impurities still exist as fine fluid or mineral inclusions. If the purification technology is improved to further remove alkali metal impurities such as Na, K, and Li from fluid or mineral inclusions, the quality can be further enhanced to above 4N6 grade. It is concluded from the study that the quartz raw material from the Kudui pluton is of excellent quality with great purification potential, meeting the quality requirements of mid-to-high-end high-purity quartz. It is confirmed by this discovery that the Northern Himalayan leucogranites possess the metallogenic potential to form large-scale high-purity quartz deposits, and this region is an important target area for seeking high-quality high-purity quartz resources.

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李煜,刘洪,胡新露,等. 北喜马拉雅淡色花岗岩中发现4N5高纯石英原料:苦堆含石榴子石二云花岗岩[J]. 科学技术与工程, , ():

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  • 收稿日期:2026-05-11
  • 最后修改日期:2026-07-04
  • 录用日期:2026-07-31
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