1. 中国地质大学(武汉)资源学院
2. 湖北省地质调查院
3. 湖北省地质勘查工程技术研究中心
4. 中国地质调查局武汉地质调查中心(中南地质科技创新中心)
纸质出版:2025
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杨紫文, 李艳军, 周豹, 等. 幕阜山复式花岗岩体西北缘伟晶岩中石榴子石成因及对Nb-Ta成矿的制约:成矿和未成矿微斜长石伟晶岩对比[J]. 地质科技通报, 2025,44(2):238-256.
杨紫文, 李艳军, 周豹, et al. 幕阜山复式花岗岩体西北缘伟晶岩中石榴子石成因及对Nb-Ta成矿的制约:成矿和未成矿微斜长石伟晶岩对比[J]. Bulletin of Geological Science and Technology, 2025, 44(2): 238-256.
杨紫文, 李艳军, 周豹, 等. 幕阜山复式花岗岩体西北缘伟晶岩中石榴子石成因及对Nb-Ta成矿的制约:成矿和未成矿微斜长石伟晶岩对比[J]. 地质科技通报, 2025,44(2):238-256. DOI: 10.19509/j.cnki.dzkq.tb20230563.
杨紫文, 李艳军, 周豹, et al. 幕阜山复式花岗岩体西北缘伟晶岩中石榴子石成因及对Nb-Ta成矿的制约:成矿和未成矿微斜长石伟晶岩对比[J]. Bulletin of Geological Science and Technology, 2025, 44(2): 238-256. DOI: 10.19509/j.cnki.dzkq.tb20230563.
江南造山带中段幕阜山地区已成为我国重要的稀有金属资源基地之一。断峰山地区伟晶岩型铌钽矿床是幕阜山复式花岗岩体西北缘唯一的大型矿床,其成因及物理化学条件不明确。新发现的微斜长石伟晶岩型铌钽矿化脉体中铌钽铁矿、石榴子石和电气石共生,其中石榴子石的成因研究可为该类型Nb-Ta成矿作用研究提供良好的制约。以断峰山地区成矿与未成矿2种微斜长石伟晶岩脉中石榴子石为研究对象,进行了背散射电子(BSE)和阴极发光(CL)微观结构观察、电子探针(EPMA)和激光电感耦合等离子质谱(LA-ICP-MS)原位微区主微量元素分析,探讨石榴子石成因及其对微斜长石伟晶岩成矿作用的指示。断峰山地区伟晶岩中的石榴子石均为岩浆成因,形成于中高温、中低压力环境,属于铁铝榴石-锰铝榴石(Alm48.61-Sps48.21)固溶体系列。成矿微斜长石伟晶岩脉中石榴子石以铁铝榴石为主(Sps42.56-Alm54.63),而未成矿微斜长石伟晶岩脉中石榴子石以锰铝榴石为主(Sps58.93-Alm37.18)。成矿微斜长石伟晶岩中石榴子石多与铌钽铁矿等共生,具有低的Mn、Nb和Ta元素含量,且由核部到边部Mn含量降低Fe含量增加,这可能是由于铌钽矿物的结晶导致,表明石榴子石中Nb、Ta、Fe、Mn等元素的演化关系可以指示幕阜山地区Nb-Ta成矿。
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