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黑色岩系型战略性关键矿产资源研究进展及主要科学问题

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本文对近年来黑色岩系型战略性关键矿产的分布规律和超常富集机制等方面的研究进展进行了归纳总结,并对战略性关键矿产资源研究进行了展望.黑色岩系分为黑色页岩、煤系地层和富碳质磷块岩等沉积地层,其中黑色页岩中发生超常富集的关键金属有Se、Te、Re、Cd、Tl等稀散金属,以及PGE、Co等稀贵金属;煤系中可见Ga和Ge的超常富集(形成独立的Ga、Ge矿床),同时也可见稀土金属、稀贵金属的富集;磷块岩中常显著富集稀土,尤其是中重稀土.黑色岩系中的关键金属主要源自大陆风化、海水、热液以及生物摄取.在风化沉积作用中,硫化-还原水体环境形成的泵吸效应,有机质的还原作用,富有机质沉积体系中有机质、铁锰氧化物、磷灰石、黏土矿物等的络合和吸附是关键金属发生富集的主要机制.黑色岩系可为热液叠加过程提供成矿金属,调节热液体系的氧逸度和硫逸度,促进超大型战略性关键矿产的形成.此外,黑色岩系富集的金属在地球层圈物质循环中的聚散行为还可对其他相关成矿系统产生影响.黑色岩系中战略性关键金属的超常富集与大陆边缘、裂谷等环境下缺氧-硫化的沉积事件相关.大气氧含量的变化、超大陆的聚合和裂解、洋流环流模式的改变、冰期以及大规模火山活动导致的海洋缺氧事件等区域地质事件均可是控制黑色岩系型战略性关键金属形成及时空分布的主要因素.黑色岩系是表生风化沉积中的一种重要类型,今后应更加重视黑色岩系等表生风化沉积作用在战略性矿产资源形成中的重要性,建立和发展相关的成矿理论.
Research progresses and main scientific issues of strategically critical minerals in black rock series
In this paper,research progresses on the distribution and supernormal enrichment mechanism of strategically critical minerals in black rock series in recent years have been summarized,and the prospect of researches on strategically critical mineral resources has been provided.The black rock series include sedimentary strata of black shale,coal-bearing strata and carbon-rich phosphorite.Especially,critical metals which were supernormally enriched in black shale include rare metals of Se,Te,Re,Cd,Tl as well as rare and precious metals of PGE,Co and others.The supernormal enrichment of Ga and Ge,commonly occurred in coal-bearing strata,led to the formation of independent Ga/Ge deposits.The enrichment of rare earth metals and rare precious metals also occurred in coal-bearing strata.Rare earth elements,particularly medium and heavy rare earth elements,were significantly enriched in phosphorites.The strategically critical metals in black rock series were mainly derived from continental weathering products,seawater,hydrothermal fluid,and the uptake of biological organisms.In the weathering and sedimentation processes,the main mechanisms responsible for the enrichment of critical metals include the pumping effect caused by the vulcanization-reduction water column,organic matter reduction,and complexation and adsorption of organic matters,iron and manganese oxides,apatite and/or clay minerals in organic-rich sedimentary systems.The black rock series can serve as a source of ore-forming metals for the hydrothermal overprinting process,regulate the oxygen and sulfur fugacities in hydrothermal systems,thereby facilitate the formation of super-large strategically critical mineral resources.In addition,it is crucial to acknowledge that metal accumulation and dispersion behaviors within the black rock series may have significant influences on other related metallogenic systems.The supernormal enrichment of strategically critical metals in black rock series is commonly associated with anoxic-vulcanization sedimentary events in continental margin and rift basin environments.Regional geological events,such as variations of atmospheric oxygen contents,the assembly and breakup of supercontinents,changes of ocean current circulation patterns,and ocean anoxia events caused by the glaciation,and large-scale volcanic activities,are likely primary factors controlling the formation and temporal and spatial distribution of strategically critical metal deposits within black rock series.The black rock series is of a significant sub-type of rocks formed through the epigenetic weathering and sedimentation process.In the future,more attention should be paid to the importance of rocks formed through the epigenetic weathering and deposition processes,such as the black rock series,in the formation of strategically critical mineral resources,and related metallogenic theories of strategically critical minerals should be established and developed.

black rock seriesstrategically critical minerals resourcessupernormal enrichment mechanismsmetallogenic process

温汉捷、周正兵、马万平、朱玉

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长安大学 地球科学与资源学院,西安 710064

中国科学院大学 地球与行星科学学院,北京 100049

东华理工大学 核资源与环境国家重点实验室,南昌 330013

黑色岩系 战略性关键矿产资源 超常富集机理 成矿过程

国家自然科学基金国家自然科学基金国家自然科学基金国家自然科学基金云南省重点研发计划

9216221441773015U181240241903037202103AQ100003

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)
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