(1.School of Earth Science and Resources,China University of Geosciences,Beijing 100083,China;
2.Henan Bureau of Non-ferrous Met allic Geology and Ores,Zhengzhou450016,China;
3.Henan Research Center for Non-ferrous Met allic Minerals Prospecting Technology,Zhengzhou 450016,China)
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[3] 杨泽强.河南商城县汤家坪钼矿辉钼矿铼-锇同位素年龄及地质意义[J].矿床地质,2007,26(3):298-295
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[6] 高阳,李永峰,郭保健,等.豫西嵩县前范岭石英脉型钼矿床地质特征及辉钼矿RE-OS同位素年龄[J].岩石学报,2010,26(3):757-767
[7] 罗正传,李永峰,王义天,等.大别山北麓河南新县大银尖钼矿床辉钼矿RE-OS同位素年龄及其意义[J].地质通报,2010,29(9):1349-1354
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[11]张兴辽.河南省重要矿产资源供需形势分析及政策建议[J].国土资源情报,2012(10):8-14
[12]何绪文,胡唤雨,胡魁.资源枯竭型城市矿产资源开发利用战略建议:以吉林省白山市浑江区为例[J].资源与产业,2013,15(1):20-24
[13]刘勤安,张兴辽.全球金融危机背景下河南钼产业发展对策研究[J].中国国土资源经济,2009(5):16-18
[14]杜科让.我国钼矿资源开采利用现状及存在的问题分析[J].科技资讯,2011(19):1-48
[15]薛亚洲,郭彤荔,余良晖,等.建立中国矿产地战略储备探讨[J].资源与产业,2011,13(2):48-52
[16]余良晖,薛亚洲,贾文龙,等.矿产地战略储备规模研究[J].资源与产业,2012,14(5):18-23