九岭地区东槽细晶岩型铌钽矿床年代学、岩石地球化学特征及其地质意义-岩石矿物学杂志-CSCIED科技核心评价数据库-手机版

九岭地区东槽细晶岩型铌钽矿床年代学、岩石地球化学特征及其地质意义

Geochronological and petrogeochemical characteristics of Dongcao aplite-type niobium-tantalum deposit in Jiuling area and their geological significance

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DOI	10.20086/j.cnki.yskw.2024.0411
刊名	岩石矿物学杂志 Acta Petrologica et Mineralogica
年，卷(期)	2024, 43(4)
作者	党飞鹏，吕川，张勇*，肖志斌，张涛，陈欣，李志鹏，汤君阳，罗建群,
作者单位	1. 核工业二七〇研究所, 江西南昌 330200; 2. 东华理工大学核资源与环境国家重点实验室, 江西南昌 330013; 3. 深层油气全国重点实验室中国石油大学(华东), 山东青岛 266580
摘要	近些年在赣西北九岭地区南部新预测了潭山－上富Nb-Ta-Li-Be成矿远景区,成矿类型包括花岗岩型和细晶岩型两类,对其进行形成时代和成因机制的研究是认识九岭地区铌、钽、锂等稀有金属富集成矿的关键。对东槽矿床含铌钽细晶岩开展了铌铁矿族矿物U-Pb年代学、岩相学和岩石地球化学研究,确定了其成岩成矿年龄、岩石成因和源区特征,并浅析其成矿潜力。结果显示,铌钽铁矿LA-ICP-MS U-Pb年龄为142±1 Ma,表明含铌钽细晶岩的成岩、成矿时代均在燕山早期(早白垩世)。含铌钽细晶岩以斜长细晶岩为主,具有富硅、富碱、富铝、低钛、贫稀土元素、Rb/Sr值变化大,富集铌、钽、锂、铷以及CaO/(K₂O+Na₂O)≤0.10、Al₂O₃/TiO₂＞160和高的分异指数(DI≥90)等特征,其稀土元素配分曲线呈弱右倾"海鸥型",微量元素蛛网图左侧隆起和右侧平缓,表明该细晶岩与强过铝质高分异S型花岗岩特征相似。综合分析认为,东槽细晶岩是九岭地区新元古界双桥山群变泥质岩在构造应力场由挤压向伸展演变的背景下发生部分熔融,并经历高程度结晶分异演化的产物。东槽含铌钽细晶岩与南岭含铌钽花岗岩、大湖塘含铌钽花岗斑岩具有相似的地球化学特征,铌、钽、锂等元素含量高,是潭山－上富成矿远景区重要的成矿地质体。
Abstract	In recent years, the Tanshan-Shangfu Nb-Ta-Li-Be metallogenic prospective area has been predicted in the southern of Jiuling area, northwest Jiangxi Province. Mineralization types include granite-type and aplite-type. Study on the formation age and genetic mechanism of rare metal deposits, is the key points of the enrichment and mineralization of rare metals in Jiuling area. Based on the study of the columbite-group minerals U-Pb geochronology, petrography and petrogeochemistry, to determine the diagenetic age and mineralization age, rock formation and magma source characters of the Nb-Ta-bearing aplite, and make analysis on its metallogenic potential. The LA-ICP-MS niobite-tantalite U-Pb dating yields an age of 142±1 Ma, suggesting that the Nb-Ta-bearing aplite was formed in the Early Yanshanian period. The aplite is characterized by rich silica, alkali and aluminum, poor titanium and ∑REE, the wide range of Rb/Sr, and there exists obvious enrichment of niobium-tantalum-lithium-rubidium, and CaO/(K₂O+Na₂O)≤0.10, Al₂O₃/TiO₂＞160, high differentiation index. The REE diagram shows rightward incline and obvious negative Eu abnormity. The spider diagram of trace elements shows left side is uplifted and right side is gentle. All of these indicate that the aplite show features of highly differentiated S-type granitoids. It may be that the metamorphic argillaceous rocks of the Neoproterozoic Shuangqiaoshan Group in the Jiuling area were partially melted to form granitic magma, which during the transition stage from syn-collision to post-collision, and then to form highly fractionated aplite. In the late stage of magmatic differentiation and evolution, the interaction between fluid and melt leads to the enrichment of metal ore-forming elements like Nb-Ta-Li in the highly fractionated aplite. The Dongcao Nb-Ta-bearing aplite and the Nanling Nb-Ta-bearing granite, the Dahutang Nb-Ta-bearing granite porphyry have similar geochemical characteristics. Which is regarded as the main metallogenic geological body in the Tanshan-Shangfu Nb-Ta-Li-Be metallogenic prospective area.
关键词	铌钽矿床；细晶岩；地球化学；铌钽铁矿U-Pb年龄；九岭地区
KeyWord	niobium-tantalum deposit; aplite; geochemistry; niobite-tantalite U-Pb age; Jiuling area
基金项目
页码	938-955

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党飞鹏，吕川，张勇*，肖志斌，张涛，陈欣，李志鹏，汤君阳，罗建群. 九岭地区东槽细晶岩型铌钽矿床年代学、岩石地球化学特征及其地质意义 [J]. 岩石矿物学杂志. 2024; 43; (4). 938 - 955.

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