ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
云南卓潘碱性杂岩体岩浆演化与稀土富集机制——来自磷灰石地球化学的证据
  
关键词:apatite  main and trace element composition  rare earth enrichment  Zhuopan alkaline complex
基金项目:国家自然科学基金项目(编号: 41963003);云南省科技计划项目(编号: 202202AG050006)
作者单位E-mail
马飞 昆明理工大学国土资源工程学院 1320049002@qq.com 
王蝶 昆明理工大学国土资源工程学院 wangdie@kust.edu.cn 
丁志丹 昆明理工大学国土资源工程学院  
刘俊鹏 昆明理工大学国土资源工程学院  
田昊丰 昆明理工大学国土资源工程学院  
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摘要:
Rare-earth Enrichment Mechanism of Magmatic Evolution in the Zhuopan Alkaline Complex, Yunnan Province:Evidence from Apatite Geochemistry
      The Zhuopan alkaline complex in Yunnan is characterized by a relatively high content of rare earth elements (REE) (approximately 1 319×10–6), showing high potential for REE exploration. However, the magmatic evolution process and the enrichment mechanism of REEs within the Zhuopan alkaline rocks warrant further investigation. This study selected the exposed lithology of the Zhuopan intrusion (syenite-pyroxenolite and gabbro-syenite), and conducted major and trace element tests on the main rare earth mineral apatite, delving into the geochemical characteristics of apatite, aiming to explore the magmatic evolution process and the mechanism of REE enrichment. The results from Electron Probe Microanalysis (EPMA) and Laser Ablation Inductively Coupled Plasma Mass Spectrometry (LA-ICP-MS) analyses indicated that the apatite found in both syenite-pyroxenolite and gabbro-syenite was fluorapatite, with fluorine contents of 2.92% and 3.31%, respectively. There were differences in the REE contents of apatite between the two rock types, with average values of 12 288×10–6 and 16 503×10–6, respectively. The REE distribution patterns for both types of apatite show an enrichment in light rare earth elements (LREEs) and a strong depletion in heavy rare earth elements (HREEs). The estimation results of the apatite Mn thermometer, combined with the relative levels of SO3 content, suggest that the oxygen fugacity in the syenite-pyroxenolite is relatively lower than that in the gabbro-syenite. The high Ce/Pb and low Th/U characteristics in apatite indicate a strong fluid activity during the magmatic evolution process, with the former exhibiting higher fluid activity than the latter. The content and ratio characteristics of volatiles (F, Cl) in apatite indicate that the magma source region was influenced by metasomatism associated with oceanic subduction. Based on the aforementioned research results, the enrichment process of rare earth elements in the Zhuopan alkaline complex can be delineated as follows: (1) During the magma chamber stage at depths of 18 to 10 kilometers, due to extensive crystallization of silicate minerals, the phosphate content in the magma chamber gradually saturates, leading to the crystallization of abundant apatite. At this point, the magma system exhibits higher fluid activity and lower volatile content, resulting in relatively lower enrichment of rare earth elements in the apatite crystallized within the syenite-pyroxenolite. (2) During the magma chamber stage at around 10 kilometers, due to the extensive crystallization of early apatite, the phosphate content decreases in the magma chamber, leading to the formation of a small amount of apatite. At this stage, the magma system exhibits lower fluid activity and higher volatile content, resulting in a higher enrichment of rare earth elements in the apatite crystallized within the gabbro-syenite. Therefore, both the syenite-pyroxenolite and gabbro-syenite in the Zhuopan alkaline complex show promising prospects for rare earth exploration to a certain extent.
MA Fei,WANG Die,DING Zhidan,LIU Junpeng,TIAN Haofeng.2024.Rare-earth Enrichment Mechanism of Magmatic Evolution in the Zhuopan Alkaline Complex, Yunnan Province:Evidence from Apatite Geochemistry[J].Acta Geoscientica Sinica,45(4):547-560.
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