中国稀土矿资源成矿地质特征与资源潜力分析
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摘要
稀土元素是元素周期表中15种镧系元素以及钪、钇等17种元素的总称。它们在材料、冶金等行业具有难以替代的作用,因而有"工业维生素"之称。作为具有战略意义的优势矿产资源之一,中国稀土资源由于近几十年的过度依赖极少数超大型矿床以及资源过度开采等问题,其占世界稀土资源储量的比重急剧下降。因此,急需进一步分析和总结其地质特征、成矿规律以及资源潜力评价。中国是世界稀土资源大国,稀土矿矿床类型齐全,前人针对其成矿理论方面也做了大量工作。本文采用矿床模型综合地质信息预测方法,在全国各省份稀土矿成矿潜力预测结果的基础之上,以MapGIS软件为平台,进行数据库汇总与综合分析研究。根据中国稀土时空分布、岩浆岩、构造和地层等控矿因素以及大地构造单元,划分了17个稀土矿成矿区带。同时,筛选出不同成因的典型矿床,总结其成矿地质特征及成矿模式。在此基础上,建立了沉积变质型、岩浆型、风化壳离子吸附型等稀土矿预测模型。在全国范围内总计圈定了930个稀土矿最小预测区,累积预测资源量约32 700×10~4 t。根据稀土矿区域成矿特征,将最小预测区归并为2级预测区,并进一步归并为133个3级预测区。此外,根据不同成矿带,按照不同预测深度、不同地质可靠程度以及不同利用程度对稀土资源量进行了汇总。最后根据稀土矿成矿地质条件,选取了广西云开大山、大寺—小董,内蒙古白云鄂博、巴尔哲,湖北庙娅—蒋家堰以及四川冕宁等6个重点的3级预测区进行资源潜力分析,为下一步勘查部署工作提供指导。
Rare earth element(REE)is a general term for the 17 elements including 15 lanthanide elements and Sc and Y.Because of its irreplaceable role in manufacturing,metallurgy and other industries,REE has earned the title of"industrial vitamin".Deemed as one of superior strategic mineral resources,the share of China's REE resource in the global reserves has declined sharply in recent decades due to over reliance on and exploitation of a few super large deposits.Therefore,it is urgent to conduct an in-depth investigation on the geological characteristics,metallogenic regularity and resource potential evaluation of REEs in China.Since it is one of the REE rich countries in the world and possesses of complete REEs,agreat deal of work has been done on REE metallogenic theory in China.Here,we carried out comprehensive analyses of REE metallogenic potential prediction of various provinces,using prediction model and comprehensive geological information prediction method with MapGIS platform.According to spatio-temporal distribution of REE deposits,and magmatite,tectonic and stratigraphic control factors,as well as tectonic units,we identified17 rare earth metallogenic zones.We also screened typical ore deposits of different genesis and summarized their geological features and metallogenic types.Further,we established prediction models of REE deposits,such as sedimentary metamorphic,magmatic and ion adsorption of weathering crust types.A total of 930 minimum prospective areas were delineated nationally,amounting to approximately 327.00 million tons of cumulative forecast REE resources.According to the regional metallogenic characteristics of REE deposits,we classified the minimum prospective areas as level-II prospective areas,which were further merged into133 level-Ⅲ prospective areas.In addition,the amount of REE resources was documented according to metallogenic belt,prediction depth,geological reliability and utilizability.We selected 6 level-Ⅲ priority prospective areas including Yunkai-Dashan and Dasi-Xiaodong in Guangxi,Bayan Obo and Baerzhe in Inner Mongolia,Miaoya-Jiangjiayan in Hubei and Mianning in Sichuan,based on metallogenic geological conditions favorable for mineral potential analysis.This work can provide guidance for further REE exploration.
Rare earth element(REE)is a general term for the 17 elements including 15 lanthanide elements and Sc and Y.Because of its irreplaceable role in manufacturing,metallurgy and other industries,REE has earned the title of"industrial vitamin".Deemed as one of superior strategic mineral resources,the share of China's REE resource in the global reserves has declined sharply in recent decades due to over reliance on and exploitation of a few super large deposits.Therefore,it is urgent to conduct an in-depth investigation on the geological characteristics,metallogenic regularity and resource potential evaluation of REEs in China.Since it is one of the REE rich countries in the world and possesses of complete REEs,agreat deal of work has been done on REE metallogenic theory in China.Here,we carried out comprehensive analyses of REE metallogenic potential prediction of various provinces,using prediction model and comprehensive geological information prediction method with MapGIS platform.According to spatio-temporal distribution of REE deposits,and magmatite,tectonic and stratigraphic control factors,as well as tectonic units,we identified17 rare earth metallogenic zones.We also screened typical ore deposits of different genesis and summarized their geological features and metallogenic types.Further,we established prediction models of REE deposits,such as sedimentary metamorphic,magmatic and ion adsorption of weathering crust types.A total of 930 minimum prospective areas were delineated nationally,amounting to approximately 327.00 million tons of cumulative forecast REE resources.According to the regional metallogenic characteristics of REE deposits,we classified the minimum prospective areas as level-II prospective areas,which were further merged into133 level-Ⅲ prospective areas.In addition,the amount of REE resources was documented according to metallogenic belt,prediction depth,geological reliability and utilizability.We selected 6 level-Ⅲ priority prospective areas including Yunkai-Dashan and Dasi-Xiaodong in Guangxi,Bayan Obo and Baerzhe in Inner Mongolia,Miaoya-Jiangjiayan in Hubei and Mianning in Sichuan,based on metallogenic geological conditions favorable for mineral potential analysis.This work can provide guidance for further REE exploration.
引文
[1]GOODENOUGH K M,SCHILLING J,JONSSON E,et al.Europe’s rare earth element resource potential[J].Ore Geology Reviews,2016,72:838-856.
[2]XIAO K,XING S,BAGAS L,et al.The China national mineral assessment initiative[J].Ore Geology Reviews,2017,91:1084-1093.
[3]BAGAS L,XIAO K,JESSELL M,et al.Quantitative assessment of China’s mineral resources(Part 1)[J].Ore Geology Reviews,2017,91:1081-1083.
[4]李建武,侯甦予.全球稀土资源分布及开发概况[J].中国国土资源经济,2012,25(5):25-27.
[5]袁忠信,李建康,王登红,等.中国稀土矿成矿规律[M].北京:地质出版社,2012.
[6]袁忠信,白鸽.中国碱性侵入岩的空间分布及有关金属矿床[J].地质与勘探,1997,33(1):44-50.
[7]王一先,赵振华.巴尔哲超大型稀土铌铍锆矿床地球化学和成因[J].地球化学,1997,26(1):24-35.
[8]袁忠信,白鸽,吴澄宇,等.内蒙白云鄂博铌、稀土、铁矿床的成矿时代和矿床成因[J].矿床地质,1991,1(1):59-70.
[9]杜小军,张强.浅析白云鄂博铁-铌-稀土矿的成矿机理[J].科技信息(科学教研),2008(24):640-641.
[10]侯宗林.白云鄂博铁-铌-稀土矿床基本地质特征成矿作用、成矿模式[J].地质与勘探,1989,25(7):1-5,22.
[11]王登红,杨建民,闫升好,等.四川牦牛坪碳酸岩的同位素地球化学及其成矿动力学[J].成都理工学院学报,2002,29(5):70-75.
[12]田世洪,丁悌平,毛景文.四川牦牛坪稀土矿床地幔流体成矿的碳、氢、氧硫同位素证据[J].地球学报,2003,24(6):543-547.
[13]刘春花,吴才来,郜源红,等.南天山拜城县波孜果尔A型花岗岩类锆石U-Pb定年及其Lu-Hf同位素组成[J].岩石学报,2014,30(6):77-96.
[14]徐海明,邹天人,方景玲,等.新疆波孜果尔铌钽矿成矿床时代及成因研究[J].矿床地质,2012,31(增刊1):625-626.
[15]SMITH M P,CAMPBELL L S,KYNICKY J.A review of the genesis of the world class Bayan Obo[J].Ore Geology Reviews,2015,64:459-476.
[16]费红彩,肖荣阁,王安建.白云鄂博REE-Nb-Fe稀土矿赋矿岩系建造研究评述[J].地质学报,2012,86(5):81-90.
[17]曹荣龙,朱寿华,王俊文.白云鄂博铁-稀土矿床的物质来源和成因理论问题[J].中国科学:B辑,1994,24(12):1298-1307.
[18]蒋明全.牦牛坪稀土矿床地质构造特征及其控矿意义[J].矿床地质,1992,11(4):351-358.
[19]陈从德,蒲广平.牦牛坪稀土矿床地质特征及其成因初探[J].地质与勘探,1991(5):18-23.
[20]徐海明,方景玲,王军,等.新疆波孜果尔铌钽矿矿床地质特征[J].矿床地质,2010,29(增刊1):309-310.
[21]祝立人,刘春根,丁少辉,等.江西省稀土矿产资源潜力评价报告[R].南昌:江西省地质调查研究院,2011.
[22]许成,宋文磊,何晨,等.外生稀土矿床的分布、类型和成因概述[J].矿物岩石地球化学通报,2015,34(2):234-241.
[23]邓茂春,曾载淋,徐九发,等.赣南离子型重稀土矿类型及找矿潜力[J].江西地质,17(2):121-127.
[24]黄典豪,吴澄宇,韩久竹.江西足洞和关西花岗岩的稀土元素地球化学及矿化特征[J].地质学报,1988(4):311-328.
[25]杨武斌,牛贺才,单强,等.巴尔哲超大型稀有稀土矿床成矿机制研究[J].岩石学报,2009,25(11):2924-2932.
[26]冯守忠.巴尔哲碱性花岗岩稀有稀土矿床地质特征及成因探讨[J].矿产与地质,1993,7(1):45-50.
[27]袁忠信,白鸽.中国内生稀有稀土矿床的时空分布[J].矿床地质,2001,20(4):53-60.
[28]吴澄宇,黄典豪,白鸽,等.南岭花岗岩类起源与稀土元素的分馏[J].岩石矿物学杂志,1990,9(2):106-116.
[29]马配学,刘在信,白鸽.广东寨背顶富重稀土花岗岩地球化学特征及岩石成因[J].河北地质学院学报,1991,14(4):351-360.
[30]谭俊,魏俊浩,李水如,等.广西昆仑关A型花岗岩地球化学特征及构造意义[J].地球科学:中国地质大学学报,2008,33(6):743-754.
[31]汪绍年.广西大容山—十万大山岩带中花岗岩类特征及成因[J].岩石学报,1991,5(2):73-80.
[32]邓希光,陈志刚,李献华,等.桂东南地区大容山—十万大山花岗岩带SHRIMP锆石U-Pb定年[J].地学评论,2004,50(4):426-432.
[33]朱金初,李向东,沈渭洲.广西花山复式花岗岩体成因的锶、钕和氧同位素研究[J].地质学报,1989(3):225-235.
[34]梁金城,邓继新,陈懋弘.桂西南早三叠世中酸性火山岩及其构造环境[J].大地构造与成矿学,2001,25(2):141-148.
[35]傅杨荣,杨昌松,陈沐龙,等.海南省稀土矿资源潜力评价成果报告[R].海口:海南省地质调查院,2011.
[36]黄典豪,吴澄宇,韩久竹,等.江西足洞和关西花岗岩体的铀-铅、铷-锶体系同位素特征及其地质意义[J].岩石学报,1989,2(1):37-48.
[37]王京彬.河岭式酸性稀土火山岩系的演化特征与稀土富集[J].中国稀土学报,1989,7(2):68-72.
[38]李石.湖北庙娅碳酸岩地球化学特征及岩石成因探讨[J].地球化学,1980(4):345-355.
[39]李石.湖北杀熊洞碳酸岩杂岩体地球化学特征及其成因探讨[J].地球化学,1991(3):245-254.
[40]黄典豪,吴澄宇,杜安道,等.东秦岭地区相矿床的铼-锇同位素年龄及其意义[J].矿床地质,1994,13(3):221-230.
[41]许成,宋文磊,漆亮,等.黄龙铺钥矿田含矿碳酸岩地球化学特征及其形成构造背景[J].岩石学报,2009,25(2):422-430.
[42]田京祥,张日田,范跃春,等.山东郗山碱性杂岩体地质特征及与稀土矿的关系[J].山东地质,2002,18(1):21-25.
[43]宋友贵,沈昆,等.鲁西南苍山县龙宝山—莲子汪地区金矿成矿规律研究及找矿靶区优选[R].济南:山东省地质科学实验研究院,1997.
[44]李培忠,于津生.黑龙江碾子山晶洞碱性花岗岩岩体年龄及其意义[J].地球化学,1993(4):389-398.
[45]张杰,朱雷,张覃.贵州织金含稀土磷块岩矿床生物成矿基本特征[J].稀土,2006,27(1):93-94.
[46]陈耀宇,朱四宏.北祁连中段与碱性岩有关的金、稀土矿床地质特征及控矿因素[J].华南地质与矿产,2001(4):45-49.
[47]吴正涛,赵呈祥,易平乾,等.青海省矿产资源潜力评价成果报告[R].西宁:青海省地质矿产勘查开发局,2013.
[48]邹天人,李庆昌.中国新疆稀有及稀土金属矿床[M].北京:地质出版社,2006.
[49]张培善.中国稀土矿床成因类型[J].地质科学,1989(1):26-32.
[50]王辑,李双庆,王保良.狼山—白云鄂博裂谷系[M].北京:北京大学出版社,1992:1-25.
[51]张宗清,袁忠信,唐索寒.白云鄂博矿床年龄和地球化学[M].北京:地质出版社,2003:148-156.
[52]裘愉卓,秦朝建,周国富,等.白云鄂博年代学新资料[C]∥第九届全国矿床会议论文集.北京:地质出版社,2009:477-479.
[53]赵景德,TATSUMOTO M,MINKIN J A,等.以多种证据建立的白云鄂博稀土矿床成矿矿物的生成顺序[J].地质找矿论丛,1991,6(4):1-17.
[54]赖小东.内蒙古白云鄂博REE-Nb-Fe矿床成因问题研究[D].合肥:中国科学技术大学,2013.
[55]骆耀南.中国攀枝花—西昌裂谷带[G]∥中国攀西裂谷文集.北京:地质出版社,1985:1-25.
[56]HOU Z Q,TIAN S H,YUAN Z X,et al.The Himalayan collision zone carbonatites in western Sichuan,SW China:petrogenesis,mantle source and tectonic implication[J].Earth and Planetary Science Letters,2006,244(1):234-250.
[57]侯增谦,田世洪,谢玉玲,等.川西冕宁—德昌喜马拉雅期稀土元素成矿带:矿床地质特征与区域成矿模型[J].矿床地质,2008,27(2):145-176.
[58]田世洪,侯增谦,杨竹森,等.川西冕宁—德昌REE成矿带成矿年代学研究:热液系统维系时限和构造控矿模型约束[J].矿床地质,2008,27(2):177-187.
[59]丘志力,梁冬云,王艳芬,等.巴尔哲碱性花岗岩锆石稀土微量元素、U-Pb年龄及其成岩成矿指示[J].岩石学报,2014,30(6):239-250.
[60]杨武斌,罗勇,单强,等.内蒙古巴尔哲稀有稀土多金属矿床特征[J].矿物学报,2009(增刊1):266.
[61]陈毓川,王登红,李厚民,等.重要矿产预测类型划分方案[M].北京:地质出版社,2008.
[2]XIAO K,XING S,BAGAS L,et al.The China national mineral assessment initiative[J].Ore Geology Reviews,2017,91:1084-1093.
[3]BAGAS L,XIAO K,JESSELL M,et al.Quantitative assessment of China’s mineral resources(Part 1)[J].Ore Geology Reviews,2017,91:1081-1083.
[4]李建武,侯甦予.全球稀土资源分布及开发概况[J].中国国土资源经济,2012,25(5):25-27.
[5]袁忠信,李建康,王登红,等.中国稀土矿成矿规律[M].北京:地质出版社,2012.
[6]袁忠信,白鸽.中国碱性侵入岩的空间分布及有关金属矿床[J].地质与勘探,1997,33(1):44-50.
[7]王一先,赵振华.巴尔哲超大型稀土铌铍锆矿床地球化学和成因[J].地球化学,1997,26(1):24-35.
[8]袁忠信,白鸽,吴澄宇,等.内蒙白云鄂博铌、稀土、铁矿床的成矿时代和矿床成因[J].矿床地质,1991,1(1):59-70.
[9]杜小军,张强.浅析白云鄂博铁-铌-稀土矿的成矿机理[J].科技信息(科学教研),2008(24):640-641.
[10]侯宗林.白云鄂博铁-铌-稀土矿床基本地质特征成矿作用、成矿模式[J].地质与勘探,1989,25(7):1-5,22.
[11]王登红,杨建民,闫升好,等.四川牦牛坪碳酸岩的同位素地球化学及其成矿动力学[J].成都理工学院学报,2002,29(5):70-75.
[12]田世洪,丁悌平,毛景文.四川牦牛坪稀土矿床地幔流体成矿的碳、氢、氧硫同位素证据[J].地球学报,2003,24(6):543-547.
[13]刘春花,吴才来,郜源红,等.南天山拜城县波孜果尔A型花岗岩类锆石U-Pb定年及其Lu-Hf同位素组成[J].岩石学报,2014,30(6):77-96.
[14]徐海明,邹天人,方景玲,等.新疆波孜果尔铌钽矿成矿床时代及成因研究[J].矿床地质,2012,31(增刊1):625-626.
[15]SMITH M P,CAMPBELL L S,KYNICKY J.A review of the genesis of the world class Bayan Obo[J].Ore Geology Reviews,2015,64:459-476.
[16]费红彩,肖荣阁,王安建.白云鄂博REE-Nb-Fe稀土矿赋矿岩系建造研究评述[J].地质学报,2012,86(5):81-90.
[17]曹荣龙,朱寿华,王俊文.白云鄂博铁-稀土矿床的物质来源和成因理论问题[J].中国科学:B辑,1994,24(12):1298-1307.
[18]蒋明全.牦牛坪稀土矿床地质构造特征及其控矿意义[J].矿床地质,1992,11(4):351-358.
[19]陈从德,蒲广平.牦牛坪稀土矿床地质特征及其成因初探[J].地质与勘探,1991(5):18-23.
[20]徐海明,方景玲,王军,等.新疆波孜果尔铌钽矿矿床地质特征[J].矿床地质,2010,29(增刊1):309-310.
[21]祝立人,刘春根,丁少辉,等.江西省稀土矿产资源潜力评价报告[R].南昌:江西省地质调查研究院,2011.
[22]许成,宋文磊,何晨,等.外生稀土矿床的分布、类型和成因概述[J].矿物岩石地球化学通报,2015,34(2):234-241.
[23]邓茂春,曾载淋,徐九发,等.赣南离子型重稀土矿类型及找矿潜力[J].江西地质,17(2):121-127.
[24]黄典豪,吴澄宇,韩久竹.江西足洞和关西花岗岩的稀土元素地球化学及矿化特征[J].地质学报,1988(4):311-328.
[25]杨武斌,牛贺才,单强,等.巴尔哲超大型稀有稀土矿床成矿机制研究[J].岩石学报,2009,25(11):2924-2932.
[26]冯守忠.巴尔哲碱性花岗岩稀有稀土矿床地质特征及成因探讨[J].矿产与地质,1993,7(1):45-50.
[27]袁忠信,白鸽.中国内生稀有稀土矿床的时空分布[J].矿床地质,2001,20(4):53-60.
[28]吴澄宇,黄典豪,白鸽,等.南岭花岗岩类起源与稀土元素的分馏[J].岩石矿物学杂志,1990,9(2):106-116.
[29]马配学,刘在信,白鸽.广东寨背顶富重稀土花岗岩地球化学特征及岩石成因[J].河北地质学院学报,1991,14(4):351-360.
[30]谭俊,魏俊浩,李水如,等.广西昆仑关A型花岗岩地球化学特征及构造意义[J].地球科学:中国地质大学学报,2008,33(6):743-754.
[31]汪绍年.广西大容山—十万大山岩带中花岗岩类特征及成因[J].岩石学报,1991,5(2):73-80.
[32]邓希光,陈志刚,李献华,等.桂东南地区大容山—十万大山花岗岩带SHRIMP锆石U-Pb定年[J].地学评论,2004,50(4):426-432.
[33]朱金初,李向东,沈渭洲.广西花山复式花岗岩体成因的锶、钕和氧同位素研究[J].地质学报,1989(3):225-235.
[34]梁金城,邓继新,陈懋弘.桂西南早三叠世中酸性火山岩及其构造环境[J].大地构造与成矿学,2001,25(2):141-148.
[35]傅杨荣,杨昌松,陈沐龙,等.海南省稀土矿资源潜力评价成果报告[R].海口:海南省地质调查院,2011.
[36]黄典豪,吴澄宇,韩久竹,等.江西足洞和关西花岗岩体的铀-铅、铷-锶体系同位素特征及其地质意义[J].岩石学报,1989,2(1):37-48.
[37]王京彬.河岭式酸性稀土火山岩系的演化特征与稀土富集[J].中国稀土学报,1989,7(2):68-72.
[38]李石.湖北庙娅碳酸岩地球化学特征及岩石成因探讨[J].地球化学,1980(4):345-355.
[39]李石.湖北杀熊洞碳酸岩杂岩体地球化学特征及其成因探讨[J].地球化学,1991(3):245-254.
[40]黄典豪,吴澄宇,杜安道,等.东秦岭地区相矿床的铼-锇同位素年龄及其意义[J].矿床地质,1994,13(3):221-230.
[41]许成,宋文磊,漆亮,等.黄龙铺钥矿田含矿碳酸岩地球化学特征及其形成构造背景[J].岩石学报,2009,25(2):422-430.
[42]田京祥,张日田,范跃春,等.山东郗山碱性杂岩体地质特征及与稀土矿的关系[J].山东地质,2002,18(1):21-25.
[43]宋友贵,沈昆,等.鲁西南苍山县龙宝山—莲子汪地区金矿成矿规律研究及找矿靶区优选[R].济南:山东省地质科学实验研究院,1997.
[44]李培忠,于津生.黑龙江碾子山晶洞碱性花岗岩岩体年龄及其意义[J].地球化学,1993(4):389-398.
[45]张杰,朱雷,张覃.贵州织金含稀土磷块岩矿床生物成矿基本特征[J].稀土,2006,27(1):93-94.
[46]陈耀宇,朱四宏.北祁连中段与碱性岩有关的金、稀土矿床地质特征及控矿因素[J].华南地质与矿产,2001(4):45-49.
[47]吴正涛,赵呈祥,易平乾,等.青海省矿产资源潜力评价成果报告[R].西宁:青海省地质矿产勘查开发局,2013.
[48]邹天人,李庆昌.中国新疆稀有及稀土金属矿床[M].北京:地质出版社,2006.
[49]张培善.中国稀土矿床成因类型[J].地质科学,1989(1):26-32.
[50]王辑,李双庆,王保良.狼山—白云鄂博裂谷系[M].北京:北京大学出版社,1992:1-25.
[51]张宗清,袁忠信,唐索寒.白云鄂博矿床年龄和地球化学[M].北京:地质出版社,2003:148-156.
[52]裘愉卓,秦朝建,周国富,等.白云鄂博年代学新资料[C]∥第九届全国矿床会议论文集.北京:地质出版社,2009:477-479.
[53]赵景德,TATSUMOTO M,MINKIN J A,等.以多种证据建立的白云鄂博稀土矿床成矿矿物的生成顺序[J].地质找矿论丛,1991,6(4):1-17.
[54]赖小东.内蒙古白云鄂博REE-Nb-Fe矿床成因问题研究[D].合肥:中国科学技术大学,2013.
[55]骆耀南.中国攀枝花—西昌裂谷带[G]∥中国攀西裂谷文集.北京:地质出版社,1985:1-25.
[56]HOU Z Q,TIAN S H,YUAN Z X,et al.The Himalayan collision zone carbonatites in western Sichuan,SW China:petrogenesis,mantle source and tectonic implication[J].Earth and Planetary Science Letters,2006,244(1):234-250.
[57]侯增谦,田世洪,谢玉玲,等.川西冕宁—德昌喜马拉雅期稀土元素成矿带:矿床地质特征与区域成矿模型[J].矿床地质,2008,27(2):145-176.
[58]田世洪,侯增谦,杨竹森,等.川西冕宁—德昌REE成矿带成矿年代学研究:热液系统维系时限和构造控矿模型约束[J].矿床地质,2008,27(2):177-187.
[59]丘志力,梁冬云,王艳芬,等.巴尔哲碱性花岗岩锆石稀土微量元素、U-Pb年龄及其成岩成矿指示[J].岩石学报,2014,30(6):239-250.
[60]杨武斌,罗勇,单强,等.内蒙古巴尔哲稀有稀土多金属矿床特征[J].矿物学报,2009(增刊1):266.
[61]陈毓川,王登红,李厚民,等.重要矿产预测类型划分方案[M].北京:地质出版社,2008.