首页|与碳酸岩-碱性岩有关的铌-稀土矿床成矿作用及成因机制

与碳酸岩-碱性岩有关的铌-稀土矿床成矿作用及成因机制

The metallogenesis and genetic mechanism of the carbonatite-alkaline rock associated niobium and rare earth element deposits

扫码查看
铌和稀土资源主要来自与碳酸岩-碱性岩相关的矿床,加强碳酸岩-碱性岩系统铌和稀土成矿作用研究,对指导我国铌和稀土资源的找矿都具有重要意义.本文对与碳酸岩-碱性岩有关的铌-稀土矿床成矿作用及成因机制进行了梳理和总结.碳酸岩-碱性岩系统中铌和稀土的初始富集一般与富集地幔的部分熔融有关,地幔源区稀土和稀有金属、碱金属和挥发分的富集是成矿的关键.橄榄石、单斜辉石等早期岩浆矿物的高度分离结晶导致残余碱性岩浆中铌和稀土的进一步富集,结晶铌和稀土矿物;碳酸岩中铌矿物结晶有堆晶岩成因和交代成因两种机制.大多数与碳酸岩-碱性岩相关的铌-稀土矿床均经历了热液蚀变,岩浆铌矿物被原地蚀变成热液铌矿物;而碳酸岩-碱性岩中矿石矿物和脉石矿物中的轻重稀土在热液过程中均可被溶解迁移再沉淀为稀土矿物.包括物理富集、化学富集和/或生物富集过程在内的地表风化过程可进一步提升碳酸岩型铌-稀土矿床的品位;在碱性硅酸岩体系中,少数矿床通过物理富集提升铌和稀土品位,而大多数矿床的风化会导致稀土矿物的分解形成一些不易被经济利用的次生稀土矿物.
Resources of niobium(Nb)and rare earth elements(REEs)are dominantly sourced from deposits associated with carbonatites and alkaline rocks.To strength the study of Nb and REEs mineralization in the carbonatite-alkaline rock system is of great significance to guide the exploration of Nb and REEs resources in China.In this paper,the mineralization and genetic mechanism of Nb-REEs deposits related to carbonatite-alkaline rocks are reviewed and summarized.The initial enrichment of Nb and REEs in the carbonatite-alkaline rock system is generally associated with the partial melting of the enriched mantle.The enrichment of rare and alkali metals and volatiles in the mantle source is the key to the Nb and REEs mineralization in the system.The high degree fractional crystallization of early-stage mgamatic minerals such as olivine and clinopyroxene resulted in the further enrichment of Nb and REEs in the residual alkaline magma,and then the crystallization of Nb and REEs minerals.The cumulate genesis and metasomatism models are two mechanisms both proposed for the formation of niobium minerals in carbonatites.Most carbonatite-alkaline rock associated Nb-REEs deposits had undergone the hydrothermal alteration.The hydrothermal niobium minerals were formed through the in-situ alteration of magmatic niobium minerals,whereas the REEs minerals were formed through the dissolution of REEs-bearing magmatic ore and gangue minerals,migration of the REEs and precipitation of new REEs minerals in the hydrothermal process.The surface weathering process,including physical enrichment,chemical enrichment,and/or biological enrichment processes,can further enhance Nb and REEs grades of ores in carbonatite type Nb-REEs deposits.The weathering of a few alkaline rock associated Nb-REEs deposits resulted in the enhancement of Nb and REEs grades of ores through the physical enrichment,whereas the weathering most alkaline rock associated Nb-REEs deposits resulted in the decomposition of hydrothermal REEs minerals and the formation of some secondary REEs minerals that are not easily and economically utilized.

carbonatitealkaline rockniobium depositREEs depositmetallogenesis

陈唯、应元灿、柳加俊、杨帆、蒋少涌

展开 >

中国地质大学(武汉) 地质过程与矿产资源国家重点实验室,紧缺战略矿产资源省部共建协同创新中心,武汉 430074

昆明理工大学 国土资源工程学院,昆明 650093

碳酸岩 碱性岩 铌矿床 稀土矿床 成矿作用

国家自然科学基金国家重点研发计划

423210012019YFA0708400

2024

矿物岩石地球化学通报
中国矿物岩石地球化学学会 中国科学院地球化学研究所

矿物岩石地球化学通报

CSTPCD北大核心
影响因子:0.912
ISSN:1007-2802
年,卷(期):2024.43(1)
  • 78