2026年第5期目录

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封面故事:西藏阿里改则县多龙矿集区拿厅铜多金属矿床深部发现世界级富金铜矿体, 封面图片展示其金品位1 g/t以上的富金铜矿体, 厚度近400 m。勘查和研究发现该铜(金)矿已成为国内第一、世界前二十的世界级富金斑岩铜多金属矿。高品位铜、金矿体赋存于黄铁绢英岩化与钾硅化蚀变过渡带, 并发育大量磁铁矿、硬石膏等指示性矿物。矿床特征与同一矿集区的 铁格隆南矿床相似, 但金品位更高, 矿床类型为斑岩-高硫化浅成低温热液叠加型矿床。正在勘查的地堡那木岗铜(金)矿是拿厅铜(金)矿体的西延部分, 经成矿预测, 拿厅—地堡那木岗铜(金)矿共伴生金将超40个大型金矿规模, 铜资源规模将超千万吨。详见本期951-959页。(图片提供: 杨超)

Cover Story:A world-class high-grade gold orebody is dis-covered at depth in the Nating porphyry copper polymetallic deposit, Duolong district, Xizang. The photo shows the high-grade gold orebody of over 1 g/t, with nearly 400 m thickness. Explo-ration and research have revealed that its gold resources have become the 1st in China and among top 20 in the world. The high-grade copper and gold orebodies occur in the transition zone be-tween phyllic alteration and potassic- silicic al-teration, and contain abundant indicator minerals such as magnetite and anhydrite. The deposit is classified as a porphyry-high sulfi-dation epithermal overprinting deposit, similar to the Tiegelongnan deposit in the Duolong dis-trict, but has a higher gold grade. The Dibaonamugang copper (gold) deposit is the western extension of the Nating orebody, fu-ture exploration will increase the associated gold resources of the Nating–Dibaonamugang copper (gold) deposit to around 40 times over large-scale gold deposit, with copper resources over 10 million tons. Therefore, the global ranking of the copper-gold resources of the Nating–Dibaonamugang deposit will be further elevated. Research on the mechanisms for gold enrichment and the modification- preservation of the deposit will be the focus of further studies. For further details, see pp. 951-959 of this issue. (Image by YANG Chao)

封面及目录  [摘要](76)[PDF](10)

西藏多龙矿集区拿厅斑岩矿床深部发现世界级富金铜矿体杨清山,杨超,夏宏伟,乔胜俊,王勤,陈红旗,董玉杰,张旺,孙豪,唐建科,甘常云,杨欢欢,周新,张琪,李玉彬,王婷婷,陈晨,陆倩茹,方向,唐菊兴  [摘要](156)[PDF](37)

莫桑比克含铜锂电气石矿物化学特征与产地示踪徐立国,吕林素,熊杰,周振华,张勇,徐明旺  [摘要](92)[PDF](8)

云南北衙超大型金多金属矿床斑岩阶段成矿流体演化——来自流体包裹体并结合H-O同位素的约束周向科,章西焕,王佳璇  [摘要](77)[PDF](8)

川西宝兴灵关晚二叠世玄武岩成因机制——对松潘—甘孜地块起源的约束李宏博,周向科,韩鎏,李常权  [摘要](84)[PDF](7)

内蒙古大杨树盆地晚白垩世含鱼生物群的发现及其意义谭锴,陈晓云,刘风香,李森乐怡  [摘要](81)[PDF](7)

龙脑香科木化石在中国新生代的首次发现程业明,王嘉树,黄路亮,刘风香  [摘要](91)[PDF](10)

中国古生代广翅鲎类(板足鲎类)化石记录及评述王嘉树,马知恒,薛进庄  [摘要](90)[PDF](6)

甘肃北山红柳河金矿床构造叠加晕模型及找矿预测陈世强,杨瑞东,戴霜,李生喜,王宁祖,李旭东,宋仁超,牛春晖  [摘要](92)[PDF](9)

甘肃加甘滩金矿覆盖层土壤微细粒地球化学指示杨冬媛,杨超,李康宁,张旺,范超楠,谢富伟,袁臻,蔡龙,白云  [摘要](92)[PDF](9)

西秦岭拉古河金矿床矿化地质特征、矿床成因及勘查指示付男,李登榜,李浩  [摘要](110)[PDF](14)

西秦岭纳合尔金矿床黄铁矿矿物化学特征及地质意义熊妍,唐菊兴,李发桥,杨涛,刘杰,邹兵,韦利莉,孟五一,尹青青,王琦,张琪  [摘要](99)[PDF](12)

云南澜沧发展河花岗岩体成因研究——锆石U-Pb年龄、地球化学及Sr-Nd-Pb同位素制约兰开军,吴亮,陈庆松,刘军平,孙建勋,魏杰,朱恩异  [摘要](83)[PDF](10)

秘鲁南部海岸岩基带基底杂岩的锆石U-Pb年龄和Lu-Hf同位素约束刘君安,郭维民,曾勇,Ccallo WALTER,Soberon DANTE,Santos ALAN  [摘要](78)[PDF](8)

西秦岭纳合尔金矿床成因——来自毒砂矿物化学及硫同位素特征的证据韦利莉,唐菊兴,邹兵,李发桥,刘杰,熊妍,张琪,孟五一,王琦,黄深川,旦增宗追  [摘要](89)[PDF](10)

青海松树南沟金矿区西矿床磁铁矿地球化学特征及成因意义叶紫枫,郎兴海,仲世新,王旭辉,董维财,罗超,李善财,王登科,李科,汤永江  [摘要](84)[PDF](8)

《地球学报》第七届编辑委员会及编辑部成员名单  [摘要](85)[PDF](15)

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