中国钼矿资源现状及国家级钼矿床实物地质资料筛选
|
摘要
根据中国钼矿床的成矿类型、成矿规模、成矿时代和分布等特点,简述了我国钼矿资源现阶段状况,提出了我国钼矿床实物地质资料筛选需要考虑的条件。结果表明:我国钼矿床类型多,以斑岩型为主,矽卡岩型次之,热液脉型、沉积型、海相火山岩型较少;我国钼矿床规模大,现阶段勘探、开发的矿床以大型、超大型矿床为主;钼矿床的成矿时代以燕山期成矿为主,其次为喜山期、印支期和海西期;钼矿床资源分布广泛,相对集中在燕辽、东秦岭、小兴安岭-张广才岭和大兴安岭4个钼矿矿集区。根据我国钼矿资源特点,结合国家实物地质资料馆馆藏规划,提出了当前符合国家实物地质资料馆收藏保管的34个钼矿床名录。
Based on the metallogenic type,metallogenic scale,metallogenic ages and distribution of molybdenum ore deposits,we summarized the current status of molybdenum ore resources in China,and proposed the considered factors when screening geological material data of molybdenum deposit.The results indicated that molybdenum ore deposit types in China were dominated by porphyry type,secondly for skarn type,hydrothermal vein type,sedimentary rock type and marine volcanic type were less.Molybdenum ore deposits were mostly large scale in China,large-size and super-large molybdenum deposits were mainly in the exploration and exploitation of molybdenum minerals at present.Metallogenic ages of molybdenum ore deposits in China were dominated by Yanshanian,followed by Himalayan period,Indo-Chinese epoch and Hercynian.Molybdenum ore resources were widely distributed but relatively centralized distributed into 4ore concentration areas,which were Yanliao,East Qinling,Xiaoxing'an Range-Zhangguangcai Range and Greater Khingan Mountains respectively.According to the characteristics of molybdenum ore resources in China,combined with schemes of National Physical Geological Data Archives,proposed 34 names of molybdenum ore deposits which fit for the current collection system construction of National Physical Geological Data Archives.
Based on the metallogenic type,metallogenic scale,metallogenic ages and distribution of molybdenum ore deposits,we summarized the current status of molybdenum ore resources in China,and proposed the considered factors when screening geological material data of molybdenum deposit.The results indicated that molybdenum ore deposit types in China were dominated by porphyry type,secondly for skarn type,hydrothermal vein type,sedimentary rock type and marine volcanic type were less.Molybdenum ore deposits were mostly large scale in China,large-size and super-large molybdenum deposits were mainly in the exploration and exploitation of molybdenum minerals at present.Metallogenic ages of molybdenum ore deposits in China were dominated by Yanshanian,followed by Himalayan period,Indo-Chinese epoch and Hercynian.Molybdenum ore resources were widely distributed but relatively centralized distributed into 4ore concentration areas,which were Yanliao,East Qinling,Xiaoxing'an Range-Zhangguangcai Range and Greater Khingan Mountains respectively.According to the characteristics of molybdenum ore resources in China,combined with schemes of National Physical Geological Data Archives,proposed 34 names of molybdenum ore deposits which fit for the current collection system construction of National Physical Geological Data Archives.
引文
[1]黄凡,王登红,王成辉,等.中国钼矿资源特征及其成矿规律概要[J].地质学报,2014,88(12):2296-2314.
[2]刘晓文,于景春,田琼.实物地质资料属性特点、重要性及研究意义[J].中国国土资源经济,2006(8):23-25.
[3]代军治,毛景文,杨富全,等.华北地台北缘燕辽钼(铜)成矿带矿床的地质特征及动力学背景[J].矿床地质,2006,25(5):598-612.
[4]付治国,靳拥护,吴飞,等.东秦岭-大别山5个特大型钼矿床的成矿母岩地质特征分析[J].地质找矿论丛,2007,22(4):277-281.
[5]黄凡,陈毓川,王登红,等.中国钼矿主要矿集区及其资源潜力探讨[J].中国地质,2011,38(5):1111-1134.
[6]毛景文,张作衡,裴荣富,等.中国矿床模型概论[M].北京:地质出版社,2012.
[7]闫兴虎,孟德明,王瑞廷,等.中国钼矿床主要类型及成矿预测[J].西北地质,2013,46(4):194-206.
[8]夏浩东,邓会娟,杨富全,等.国家级矿产实物地质资料的筛选和管理意义[J].地质通报,2005,24(10-11):1069-1073.
[9]王京彬,邹滔,王玉往,等.中国钼多金属矿床的组合类型、成矿作用和成矿谱系[J].矿床地质,2014,33(3):447-470.
[10]石小琛.中国钼矿资源评估与开发可行性研究[D].北京:中国地质大学(北京),2010.
[11]杨言辰,韩世炯,孙德有,等.小兴安岭-张广才岭成矿带斑岩型钼矿床岩石地球化学特征及其年代学研究[J].岩石学报,2012,28(2):379-390.
[12]杨岳清,赵金花,孟贵祥,等.内蒙古北山地区斑岩型钼矿的成岩成矿时代和形成环境探讨[J].地球学报,2013,34(4):401-412.
[13]邓晋福,赵国春,赵海玲,等.中国东部燕山期火成岩构造组合与造山—深部过程[J].地质评论,2000,46(1):41-48.
[14]尹煜春.内蒙古乌奴格吐山次火山斑岩型铜-钼矿床控矿因素分析及找矿方向[J].矿产与地质,2007,21(3):298-303.
[15]陈志广,张连昌,卢百志,等.内蒙古太平川铜钼矿成矿斑岩时代、地球化学及地质意义[J].岩石学报,2010,26(5):1437-1449.
[16]聂凤军,孙振江,李超,等.黑龙江岔路口钼多金属矿床辉钼矿铼-锇同位素年龄及地质意义[J].矿产与地质,2011,30(5):828-836.
[17]卢贺,孙靖宇,赵泽龙.内蒙古太平沟斑岩型铜钼矿床地质特征及找矿方向探讨[J].新疆有色金属,2013(3):25-28.
[18]李向文,王可勇,钱烨,等.吉林大黑山钼矿床成矿流体地球化学特征及其地质意义[J].岩石学报,2013,29(9):3173-3182.
[19]史致元,王玉增,孟广才,等.吉林省舒兰季德屯大型钼矿床地质特征及找矿过程中化探异常查证效果[J].岩石学报,2010,29(1):62-65.
[20]谭红艳,舒广龙,吕骏超,等.小兴安岭鹿鸣大型钼矿LA-ICPMS锆石U-Pb和辉钼矿Re-Os年龄及其地质意义[J].吉林大学学报:地球科学版,2012,42(6):1757-1770.
[21]刘晓林,范平,郑志丰,等.辽西杨家杖子八家子钼多金属成矿带—典型钼矿床特征及找矿远景预测[J].地质与资源,2009,18(2):110-115.
[22]魏然,王建国,王义天,王圣文.河北省撒岱沟门斑岩型钼矿床二长花岗岩的锆石U-Pb年龄及其意义[J].中国地质,2013,40(6):1736-1748.
[23]聂凤军,李香资,李超,等.内蒙古兴和县曹四夭特大型钼矿床辉钼矿Re-Os同位素年龄及地质意义[J].地质调查与研究,2013,59(1):175-181.
[24]张彤,陈志勇,许立权,等.内蒙古卓资县大苏计钼矿辉钼矿铼-锇同位素定年及其地质意义[J].岩矿测试,2009,28(3):279-282.
[25]丁正江,孙丰月,刘建辉,等.胶东邢家山钼钨矿床辉钼矿Re-Os同位素测年及其地质意义[J].岩石学报,2012,28(9):2721-2732.
[26]徐刚,汤中立,焦建刚,等.金堆城与沙坪沟小岩体型斑岩钼矿床对比研究[J].西北地质,2012,45(4):357-369.
[27]黄典豪,侯增谦,杨志明,等.东秦岭钼矿带内碳酸岩脉型钼(铅)矿床地质-地球化学特征、成矿机制及成矿构造背景[J].地质学报,2009,83(12):1968-1984.
[28]李永峰,毛景文,胡华斌,等.东秦岭钼矿类型、特征、成矿时代及其地球动力学背景[J].矿床地质,2005.24(3):292-304.
[29]付治国,宋要武,鲁玉红.河南汝阳东沟钼矿床控矿地质条件及综合找矿信息[J].地质与勘探,2006,42(2):33-28.
[30]孟祥金,徐文艺,吕庆田,等.安徽沙坪沟斑岩钼矿锆石U-Pb和辉钼矿Re-Os年龄[J].地质学报,2012.86(3):486-494.
[31]文春华,徐文艺,钟宏,等.九瑞矿集区城门山斑岩型钼铜矿床流体包裹体研究[J].地质学报,2012,86(10):1604-1620.
[32]刘玄,范宏瑞,胡芳芳,等.江西德兴斑岩铜钼矿床流体包裹体子矿物SEM-EDS研究及其对成矿流体性质的制约[J].岩石学报,2011,27(5):1397-1409.
[33]黄凡,王登红,曾载淋,等.赣南园岭寨大型钼矿岩石地球化学、成岩成矿年代学及其地质意义[J].大地构造与成矿学,2012,36(3):363-376.
[34]刘莎,王春龙,黄文婷,等.粤北大宝山斑岩钼钨矿床赋矿岩体锆石LA-ICP-MS U-Pb年龄与矿床形成动力学背景分析[J].大地构造与成矿学,2012,36(3):440-449.
[35]肖广玲,孙晓雁,王启,等.浙东南石平川钼矿床地质特征、成矿时代及成因[J].地质科技情报,2010,29(1):74-85.
[36]石礼炎.福建古田西朝钼矿床成矿构造特征及找矿方向[J].福建地质,2009,3(28):167-174.
[37]王国君,刘君,曹玉莲,等.海南罗葵洞斑岩型钼矿地质特征及矿床成因[J].矿床勘查,2010,1(5):453-457.
[38]栗亚芝,宋忠宝,杜玉良,等.纳日贡玛斑岩型铜钼矿与玉龙斑岩铜矿成矿特征对比研究[J].西北地质,2012,45(1):149-157.
[39]唐菊兴,陈毓川,王登红,等.西藏工布江达县沙让斑岩钼矿床辉钼矿铼-锇同位素年龄及其地质意义[J].地质学报,2009,83(5):698-704.
[40]彭振安,李红红,屈文俊,等.内蒙古北山地区小狐狸山钼矿床辉钼矿Re-Os同位素年龄及其地质意义[J].矿床地质,2010,29(3):510-516.
[41]涂其军,董连慧,王克卓.东天山东戈壁钼矿辉钼矿Re-Os同位素年龄及地质意义[J].新疆地质,2012,30(3):272-276.
[42]蔡明海,彭振安,屈文俊,等.内蒙古乌拉特后旗查干德尔斯钼矿床地质特征及Re-Os测年[J].矿床地质,2011,30(3):377-384.
[43]宋史刚,丁振举,姚书振,等.甘肃武山温泉辉钼矿Re-Os同位素定年及其成矿意义[J].西北地质,2008,41(1):67-73.
[44]刘文均.四川沐川含钼啥岩中钼赋存状态及沐川矿分布规律的研究[J].矿物岩石,1985(1):104-110.
[45]周洁,胡凯.贵州遵义下寒武统黑色页岩镍、钼多金属矿床的形态硫特征及成矿模式[J].资源调查与环境,2008,29(2):87-91.
[2]刘晓文,于景春,田琼.实物地质资料属性特点、重要性及研究意义[J].中国国土资源经济,2006(8):23-25.
[3]代军治,毛景文,杨富全,等.华北地台北缘燕辽钼(铜)成矿带矿床的地质特征及动力学背景[J].矿床地质,2006,25(5):598-612.
[4]付治国,靳拥护,吴飞,等.东秦岭-大别山5个特大型钼矿床的成矿母岩地质特征分析[J].地质找矿论丛,2007,22(4):277-281.
[5]黄凡,陈毓川,王登红,等.中国钼矿主要矿集区及其资源潜力探讨[J].中国地质,2011,38(5):1111-1134.
[6]毛景文,张作衡,裴荣富,等.中国矿床模型概论[M].北京:地质出版社,2012.
[7]闫兴虎,孟德明,王瑞廷,等.中国钼矿床主要类型及成矿预测[J].西北地质,2013,46(4):194-206.
[8]夏浩东,邓会娟,杨富全,等.国家级矿产实物地质资料的筛选和管理意义[J].地质通报,2005,24(10-11):1069-1073.
[9]王京彬,邹滔,王玉往,等.中国钼多金属矿床的组合类型、成矿作用和成矿谱系[J].矿床地质,2014,33(3):447-470.
[10]石小琛.中国钼矿资源评估与开发可行性研究[D].北京:中国地质大学(北京),2010.
[11]杨言辰,韩世炯,孙德有,等.小兴安岭-张广才岭成矿带斑岩型钼矿床岩石地球化学特征及其年代学研究[J].岩石学报,2012,28(2):379-390.
[12]杨岳清,赵金花,孟贵祥,等.内蒙古北山地区斑岩型钼矿的成岩成矿时代和形成环境探讨[J].地球学报,2013,34(4):401-412.
[13]邓晋福,赵国春,赵海玲,等.中国东部燕山期火成岩构造组合与造山—深部过程[J].地质评论,2000,46(1):41-48.
[14]尹煜春.内蒙古乌奴格吐山次火山斑岩型铜-钼矿床控矿因素分析及找矿方向[J].矿产与地质,2007,21(3):298-303.
[15]陈志广,张连昌,卢百志,等.内蒙古太平川铜钼矿成矿斑岩时代、地球化学及地质意义[J].岩石学报,2010,26(5):1437-1449.
[16]聂凤军,孙振江,李超,等.黑龙江岔路口钼多金属矿床辉钼矿铼-锇同位素年龄及地质意义[J].矿产与地质,2011,30(5):828-836.
[17]卢贺,孙靖宇,赵泽龙.内蒙古太平沟斑岩型铜钼矿床地质特征及找矿方向探讨[J].新疆有色金属,2013(3):25-28.
[18]李向文,王可勇,钱烨,等.吉林大黑山钼矿床成矿流体地球化学特征及其地质意义[J].岩石学报,2013,29(9):3173-3182.
[19]史致元,王玉增,孟广才,等.吉林省舒兰季德屯大型钼矿床地质特征及找矿过程中化探异常查证效果[J].岩石学报,2010,29(1):62-65.
[20]谭红艳,舒广龙,吕骏超,等.小兴安岭鹿鸣大型钼矿LA-ICPMS锆石U-Pb和辉钼矿Re-Os年龄及其地质意义[J].吉林大学学报:地球科学版,2012,42(6):1757-1770.
[21]刘晓林,范平,郑志丰,等.辽西杨家杖子八家子钼多金属成矿带—典型钼矿床特征及找矿远景预测[J].地质与资源,2009,18(2):110-115.
[22]魏然,王建国,王义天,王圣文.河北省撒岱沟门斑岩型钼矿床二长花岗岩的锆石U-Pb年龄及其意义[J].中国地质,2013,40(6):1736-1748.
[23]聂凤军,李香资,李超,等.内蒙古兴和县曹四夭特大型钼矿床辉钼矿Re-Os同位素年龄及地质意义[J].地质调查与研究,2013,59(1):175-181.
[24]张彤,陈志勇,许立权,等.内蒙古卓资县大苏计钼矿辉钼矿铼-锇同位素定年及其地质意义[J].岩矿测试,2009,28(3):279-282.
[25]丁正江,孙丰月,刘建辉,等.胶东邢家山钼钨矿床辉钼矿Re-Os同位素测年及其地质意义[J].岩石学报,2012,28(9):2721-2732.
[26]徐刚,汤中立,焦建刚,等.金堆城与沙坪沟小岩体型斑岩钼矿床对比研究[J].西北地质,2012,45(4):357-369.
[27]黄典豪,侯增谦,杨志明,等.东秦岭钼矿带内碳酸岩脉型钼(铅)矿床地质-地球化学特征、成矿机制及成矿构造背景[J].地质学报,2009,83(12):1968-1984.
[28]李永峰,毛景文,胡华斌,等.东秦岭钼矿类型、特征、成矿时代及其地球动力学背景[J].矿床地质,2005.24(3):292-304.
[29]付治国,宋要武,鲁玉红.河南汝阳东沟钼矿床控矿地质条件及综合找矿信息[J].地质与勘探,2006,42(2):33-28.
[30]孟祥金,徐文艺,吕庆田,等.安徽沙坪沟斑岩钼矿锆石U-Pb和辉钼矿Re-Os年龄[J].地质学报,2012.86(3):486-494.
[31]文春华,徐文艺,钟宏,等.九瑞矿集区城门山斑岩型钼铜矿床流体包裹体研究[J].地质学报,2012,86(10):1604-1620.
[32]刘玄,范宏瑞,胡芳芳,等.江西德兴斑岩铜钼矿床流体包裹体子矿物SEM-EDS研究及其对成矿流体性质的制约[J].岩石学报,2011,27(5):1397-1409.
[33]黄凡,王登红,曾载淋,等.赣南园岭寨大型钼矿岩石地球化学、成岩成矿年代学及其地质意义[J].大地构造与成矿学,2012,36(3):363-376.
[34]刘莎,王春龙,黄文婷,等.粤北大宝山斑岩钼钨矿床赋矿岩体锆石LA-ICP-MS U-Pb年龄与矿床形成动力学背景分析[J].大地构造与成矿学,2012,36(3):440-449.
[35]肖广玲,孙晓雁,王启,等.浙东南石平川钼矿床地质特征、成矿时代及成因[J].地质科技情报,2010,29(1):74-85.
[36]石礼炎.福建古田西朝钼矿床成矿构造特征及找矿方向[J].福建地质,2009,3(28):167-174.
[37]王国君,刘君,曹玉莲,等.海南罗葵洞斑岩型钼矿地质特征及矿床成因[J].矿床勘查,2010,1(5):453-457.
[38]栗亚芝,宋忠宝,杜玉良,等.纳日贡玛斑岩型铜钼矿与玉龙斑岩铜矿成矿特征对比研究[J].西北地质,2012,45(1):149-157.
[39]唐菊兴,陈毓川,王登红,等.西藏工布江达县沙让斑岩钼矿床辉钼矿铼-锇同位素年龄及其地质意义[J].地质学报,2009,83(5):698-704.
[40]彭振安,李红红,屈文俊,等.内蒙古北山地区小狐狸山钼矿床辉钼矿Re-Os同位素年龄及其地质意义[J].矿床地质,2010,29(3):510-516.
[41]涂其军,董连慧,王克卓.东天山东戈壁钼矿辉钼矿Re-Os同位素年龄及地质意义[J].新疆地质,2012,30(3):272-276.
[42]蔡明海,彭振安,屈文俊,等.内蒙古乌拉特后旗查干德尔斯钼矿床地质特征及Re-Os测年[J].矿床地质,2011,30(3):377-384.
[43]宋史刚,丁振举,姚书振,等.甘肃武山温泉辉钼矿Re-Os同位素定年及其成矿意义[J].西北地质,2008,41(1):67-73.
[44]刘文均.四川沐川含钼啥岩中钼赋存状态及沐川矿分布规律的研究[J].矿物岩石,1985(1):104-110.
[45]周洁,胡凯.贵州遵义下寒武统黑色页岩镍、钼多金属矿床的形态硫特征及成矿模式[J].资源调查与环境,2008,29(2):87-91.