关键矿产的研究意义、矿种厘定、资源属性、找矿进展、存在问题及主攻方向
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摘要
自工业4.0和第四次科技革命开始以来,关键矿产的重要性越来越显著。2017年底,特朗普以总统令的方式要求美国对35种危机矿产实现"自给",进一步提升了国际社会对于关键矿产的关注度。中国作为世界上最大的发展中国家,但矿产资源的自给能力远不如美国,不但大宗矿产需要大量进口,锂铍铌钽等稀有金属的对外依存度也是居高不下,而中国社会对于这些"小矿种"的重视程度也远不如美国。因此,加强对关键矿产的调查研究与找矿勘查已经迫在眉睫。在当前形势下,为了保障战略性新兴产业的发展,为了实现伟大复兴的中国梦,也为了国民经济和国家的长治久安,提出将9种稀有金属、17种稀土金属、8种稀散金属、6种稀贵金属、3种稀有气体矿产、12种关键黑色和有色金属矿产和8种非金属矿产及铀作为中国的关键矿产。这8个大类41个矿种(组)与美国的35个矿种(组)大致对应。自2011年以来,中国以稀有稀土稀散金属(三稀)矿产为重点开展了调查评价工作,在成矿理论、潜力评价、找矿突破、环境保护、物理选矿、找矿方法、分析测试、矿政管理等方面不断取得新进展,尤其是通过对四川甲基卡及可尔因等地的找矿工作,新增资源储量相当于10个大型锂辉石矿床,为川西大型锂矿资源基地的建设提供了资源保障。但是,我国铌钽铍等长期短缺的稀有金属仍然没有取得找矿突破,以往探明的资源往往品位低、难选冶而实际上有相当一部分资源属于"呆矿";即便是以往具有优势的锡、锑、汞等有色金属也已经开始进口,湖南锡矿山等世界闻名的大型超大型矿床纷纷进入资源枯竭阶段,接替资源难以为继,需要高度重视。建议在加强已有矿山深部找矿的同时,不但要继续攻克共伴生资源综合利用的难题,还要对非常规的、新类型的关键矿产资源(如沉积型锂矿)加强研究、勘查与开发利用的攻关,从关键矿产的关键应用方面寻找突破口,让关键矿产在关键时刻发挥关键作用。
Since the start of the industrial 4.0 and the fourth technological revolution, the importance of critical mineral resources has become increasingly prominent. At the end of 2017, Trump, by presidential decree, demanded that the United States "be self-sufficient" of 35 kinds critical minerals. Further increased international attention to critical mineral resources. As the largest developing country in the world, China is far less self-supporting than the United States in terms of mineral resources. Not only do large quantities of minerals need to be imported, but the externaldependence of rare metals such as lithium, beryllium, niobium, tantalum and other rare metals is also high. And Chinese society attaches less importance to these "little minerals" than the United States. Therefore, the investigation and research of critical mineral resources should be strengthened. Exploration and prospecting are imminent. Under the current situation, in order to ensure the development of strategic emerging industries, in order to achieve the great rejuvenation of Chinese Dream, and for the long-term stability of the national economy and the country, this paper proposes that 9 kinds of rare metals, 17 kinds of rare earth metals, 8 kinds of scattered metals, 3 kinds of rare gas, 12 kinds of traditional metals(black and non-ferrous), 8 kinds of non-metallic minerals and uranium, should be put forward and determinated as the critical mineral resources in China. These 8 groups of 41 kinds of mineral resources correspond roughly to the 35 kinds of minerals in the United States. Since 2011, China has focused on rare metals, rare earths and rare scatted metals(so called as rrr metals or 3 R) minerals. New progress has been made in the fields of metallogenic theory, potential evaluation, ore prospecting breakthrough, environmental protection, mineral processing by physical methods, ore prospecting methods, analysis and testing, and mining administration, etc. In particular, through the prospecting of Jiajika and Keyin in Sichuan Province, the potential of new resources is equal to 10 large spodumene deposits, which provides a resource guarantee for the construction of large lithium ore resource base in western Sichuan. However, China's long-term shortage of rare metals, such as niobium, tantalum and beryllium, has not yet made a breakthrough in prospecting. In the past, proven resources are often of low grade and difficult to be cleaned and smelted. In fact, a considerable portion of resources belong to "dull ore"; even tin, which used to have advantages in the past, Non-ferrous metals such as antimony, mercury and other non-ferrous metals have also begun to import, the Xikuangshan Sb mine and other world-famous large-scale and super-large-scale deposits have entered the stage of resource depletion, it is difficult to replace resources, and needs to be attached great importance. It is suggested that while strengthening the deep prospecting of existing mines, we should not only continue to overcome the difficult problem of comprehensive utilization of co-associated resources, but also strengthen the research and exploration of unconventional and new types of critical mineral resources(such as the lithium resources associated with sedimentary rocks). We should strengthen the basic research, find a breakthrough in the critical application of the critical mineral resources, and let the critical mineral resources play a critical role at the critical moment.
Since the start of the industrial 4.0 and the fourth technological revolution, the importance of critical mineral resources has become increasingly prominent. At the end of 2017, Trump, by presidential decree, demanded that the United States "be self-sufficient" of 35 kinds critical minerals. Further increased international attention to critical mineral resources. As the largest developing country in the world, China is far less self-supporting than the United States in terms of mineral resources. Not only do large quantities of minerals need to be imported, but the externaldependence of rare metals such as lithium, beryllium, niobium, tantalum and other rare metals is also high. And Chinese society attaches less importance to these "little minerals" than the United States. Therefore, the investigation and research of critical mineral resources should be strengthened. Exploration and prospecting are imminent. Under the current situation, in order to ensure the development of strategic emerging industries, in order to achieve the great rejuvenation of Chinese Dream, and for the long-term stability of the national economy and the country, this paper proposes that 9 kinds of rare metals, 17 kinds of rare earth metals, 8 kinds of scattered metals, 3 kinds of rare gas, 12 kinds of traditional metals(black and non-ferrous), 8 kinds of non-metallic minerals and uranium, should be put forward and determinated as the critical mineral resources in China. These 8 groups of 41 kinds of mineral resources correspond roughly to the 35 kinds of minerals in the United States. Since 2011, China has focused on rare metals, rare earths and rare scatted metals(so called as rrr metals or 3 R) minerals. New progress has been made in the fields of metallogenic theory, potential evaluation, ore prospecting breakthrough, environmental protection, mineral processing by physical methods, ore prospecting methods, analysis and testing, and mining administration, etc. In particular, through the prospecting of Jiajika and Keyin in Sichuan Province, the potential of new resources is equal to 10 large spodumene deposits, which provides a resource guarantee for the construction of large lithium ore resource base in western Sichuan. However, China's long-term shortage of rare metals, such as niobium, tantalum and beryllium, has not yet made a breakthrough in prospecting. In the past, proven resources are often of low grade and difficult to be cleaned and smelted. In fact, a considerable portion of resources belong to "dull ore"; even tin, which used to have advantages in the past, Non-ferrous metals such as antimony, mercury and other non-ferrous metals have also begun to import, the Xikuangshan Sb mine and other world-famous large-scale and super-large-scale deposits have entered the stage of resource depletion, it is difficult to replace resources, and needs to be attached great importance. It is suggested that while strengthening the deep prospecting of existing mines, we should not only continue to overcome the difficult problem of comprehensive utilization of co-associated resources, but also strengthen the research and exploration of unconventional and new types of critical mineral resources(such as the lithium resources associated with sedimentary rocks). We should strengthen the basic research, find a breakthrough in the critical application of the critical mineral resources, and let the critical mineral resources play a critical role at the critical moment.
引文
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王登红.2018.关键矿产资源的成矿规律、找矿勘查与物质循环(2018-12-8,成都双清论坛多媒体).
王登红,陈毓川,徐志刚,李天德,傅旭杰.2002.阿尔泰成矿省的成矿系列及成矿规律研究.北京:原子能出版社,1～493.
王登红,邹天人,徐志刚,余金杰,付小方.2004.伟晶岩矿产示踪造山过程的研究进展.地球科学进展,19(4):614～620.
王登红,唐菊兴,应立娟,陈郑辉,许建祥,张家菁,李水如,曾载淋.2010.“五层楼+地下室”找矿模型的适用性及其对深部找矿的意义.吉林大学学报(地球科学版),40(4):733～738.
王登红,李立兴,李建康,李晓妹,郑国栋,于扬,赵芝.2012a.海洋稀土资源及其对中国稀土产业的可能影响.矿床地质,31(增刊):1109～1110.
王登红,王瑞江,李建康,赵芝,于扬,郑国栋,李晓妹,孙艳,李德先,赵汀.2012b.我国三稀矿产资源基本特征与研究现状.矿床地质,31(增刊):41～42.
王登红,付小方.2013a.四川甲基卡外围锂矿找矿取得突破.岩矿测试,32(6):987.
王登红,李沛刚,屈文俊,雷志远,廖友常.2013b.贵州大竹园铝土矿中钨和锂的发现与综合评价.中国科学:地球科学,43(1):44 ～51.
王登红,王瑞江,李建康,赵芝,于扬,代晶晶,陈郑辉,李德先,屈文俊,邓茂春,付小方,孙艳,郑国栋.2013c.中国三稀矿产资源战略调查研究进展综述.中国地质,40(2):361～370.
王登红,赵芝,于扬,赵汀,李建康,代晶晶,刘新星何晗晗.2013d.离子吸附型稀土资源研究进展、存在问题及今后研究方向.岩矿测试,32(5):796～802.
王登红,徐志刚,盛继福,朱明玉,徐珏,袁忠信,白鸽,屈文俊,李华芹,陈郑辉,王成辉,黄凡,张长青,王永磊,应立娟,李厚民,高兰,孙涛,付勇,李建康,武广,唐菊兴,丰成友,赵正,张大权.2014.全国重要矿产和区域成矿规律研究进展综述.地质学报,88(12):2176～2191.
王登红,刘丽君,刘新星,赵芝,何晗晗.2016a.我国能源金属矿产的主要类型及发展趋势探讨.桂林理工大学学报,36(1):21～29.
王登红,王瑞江,付小方,孙艳,王成辉,郝雪峰,刘丽君,潘蒙,侯江龙,代晶晶,田世洪,于扬.2016b.对能源金属矿产资源基地调查评价基本问题的探讨——以四川甲基卡大型锂矿基地为例.地球学报,37(4):471～480.
王登红,王瑞江,李建康,赵芝,孙艳,于扬,赵汀,代晶晶,王成辉,黄凡,刘丽君,代鸿章.2016c.新兴产业的发展与三稀矿产的调查.地质论评,62(增刊):423～425.
王登红,王瑞江,孙艳,李建康,赵芝,赵汀,屈文俊,付小方,江善元,黄华谷,冯文杰,徐平,李胜苗,黄新鹏,周辉,朱永新,涂其军,李新仁,方一平,周园园.2016d.我国三稀(稀有稀土稀散)矿产资源调查研究成果综述.地球学报,37(5):587～598.
王登红,赵汀,何晗晗,刘新星,刘祥,黄华谷.2016e.中南地区三稀矿产资源调查研究及开发利用进展综述.桂林理工大学学报,36(1):1～8.
王登红,刘丽君,代鸿章,刘善宝,侯江龙,吴西顺.2017a.试论国内外大型超大型锂辉石矿床的特殊性与找矿方向.地球科学,42(12):1～15.
王登红,刘丽君,侯江龙,代鸿章,于扬,代晶晶,田世洪.2017b.初论甲基卡式稀有金属矿床“五层楼+地下室”勘查模型.地学前缘,24(5):1～7.
王登红,王成辉,孙艳,李建康,刘善宝,饶魁元.2017c.我国锂铍钽矿床调查研究进展及相关问题简述.中国地质调查,4(5):1～8.
王登红,吴西顺.2017d.21世纪的能源金属——锂的奥秘.国土资源科普与文化,(4):22～27.
王登红,赵芝,于扬,王成辉,代晶晶,孙艳,赵汀,李建康,黄凡,陈振宇,曾载淋,邓茂春,邹新勇,黄华谷,周辉,冯文杰.2017e.我国离子吸附型稀土矿产科学研究和调查评价新进展.地球学报,38(3):317～325.
王登红,李建康,李建国,赵斌,周四春,梁婷,王汝成,屈文俊,魏彪,梁华英,许以明,周新鹏,张荣华,王永磊,秦燕,何晗晗,李超,龚述清,张怡军,单强,韦龙明,林锦富,汪林峰.2018a.南岭成矿带深部探测的理论与实践.北京:地质出版社,1～471.
王登红,孙艳,刘喜方,田世洪,代晶晶,刘丽君,代鸿章.2018b.锂能源金属矿产深部探测技术方法与找矿方向.中国地质调查,5(1):1～9.
王登红,章少华,熊先孝,王永磊,王成辉,王志强,王淑丽,付勇,刘玉芹,刘丽君,刘新星,江彪,孙小虹,孙艳,孙涛,李立兴,李建康,李超,杨刚,吴先冰,何晗晗,应立娟,张长青,陈郑辉,陈振宇,郑玉琴,郑厚义,孟凡,赵正,赵芝,侯江龙,郭春丽,黄凡,曹承立,曹烨,梁婷,詹建华,颜玲亚.2018c.中国矿产地质志·典型矿床总述卷.北京:地质出版社,1～1177.
王登红,孙艳,代鸿章,郭唯明,赵芝,李建康,王成辉,黄凡,于扬,李德先.2019.我国“三稀矿产”的资源特征及开发利用研究.中国工程科学,21(1):119～127.
王瑞江,王登红,李建康,孙艳,李德先,郭春丽,赵芝,于扬,黄凡,王成辉,刘家军,何晗晗,郑国栋,黄文斌,周园园,李晓妹,刘丽君,蔡肖,赵汀,宋扬.2015.稀有稀土稀散矿产资源及其开发利用.北京:地质出版社,1～429.
熊欣,李建康,王登红,刘丽君,代鸿章.2019.川西甲基卡花岗伟晶岩型锂矿床中熔体、流体包裹体固相物质研究.岩石矿物学杂志,38(2):241～253.
于扬,王登红,田兆雪,黄凡,赵芝,孙艳,李德先,何晗晗,邓茂春.2017.稀土矿区环境调查SMAIMA方法体系、评价模型及其应用——以赣南离子吸附型稀土矿山为例.地球学报,38(3):335～344.
于扬,王登红,高娟琴,刘丽君,王伟,张塞.2019.中国三稀矿产生物找矿技术方法及其应用综述.地质学报,93(6):1533～1542.
余韵,陈甲斌.2017.美国危机矿产研究概况及其启示.国土资源情报,(2):45～51.
袁忠信,何晗晗,刘丽君,王登红,赵芝.2016,国外稀有稀土矿床.北京:中国科学出版社,170.
赵汀,王登红,王瑞江,邓茂春,陈为光.2014.克里格法在离子吸附型稀土矿勘查储量估算中的应用.岩矿测试,33(1):126～133.
赵汀,王登红,黄文斌,李晓妹,郑国栋,孙艳,于扬.2016.三稀战略调查成果数据库建设与应用.桂林理工大学学报,36(1):36～41.
赵汀,王登红,刘超,李德先,周凤英.2019.中国锗矿成矿规律与开发利用现状.地质学报,93(6):1245～1251.
赵芝,付小方,任希杰,方一平,侯立玮,王登红,刘丽君.2013.四川稀土精矿的稀土元素和微量元素地球化学特征及开发利用意义.岩矿测试,32(5):810～816.
赵芝,王登红,陈郑辉,陈振宇.2017,南岭离子吸附型稀土矿床成矿规律研究新进展.地质学报,91(12):2814～2827.
赵芝,王登红,王成辉,王臻,邹新勇,冯文杰,周辉,黄新鹏,黄华谷.2019.离子吸附型稀土找矿及研究新进展.地质学报,93(6):1454～1465.
周芳春,李建康,刘翔,李鹏,黄志飚,石威科,苏俊男,陈虎,黄小强.2019.湖南仁里铌钽矿床矿体地球化学特征及其成因意义.地质学报,93(6):1392～1404.
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