| 钼的地球化学性质与成矿 |
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| 引用本文： | 孙卫东,李聪颖,凌明星,丁兴,杨晓勇,梁华英,张红,范蔚茗.钼的地球化学性质与成矿[J].岩石学报,2015,31(7):1807-1817. |
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| 作者姓名： | 孙卫东 李聪颖 凌明星 丁兴 杨晓勇 梁华英 张红 范蔚茗 |
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| 作者单位： | 中国科学院广州地球化学研究所, 中国科学院矿物与成矿重点实验室, 广州 510640;中国科学院青藏高原地球科学卓越创新中心, 北京 100101,中国科学院广州地球化学研究所, 中国科学院矿物与成矿重点实验室, 广州 510640,中国科学院广州地球化学研究所, 中国科学院同位素年代学和地球化学重点实验室, 广州 510640,中国科学院广州地球化学研究所, 中国科学院同位素年代学和地球化学重点实验室, 广州 510640,中国科学技术大学地球和空间科学学院, 合肥 230026,中国科学院广州地球化学研究所, 中国科学院矿物与成矿重点实验室, 广州 510640,西北大学地质学系, 西安 710069,中国科学院青藏高原地球科学卓越创新中心, 北京 100101 |
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| 基金项目： | 本文受科技部973项目(2012CB416703)和国家自然科学基金项目(41090374、41121002)联合资助. |
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| 摘 要： | 钼在硅酸盐地球中的丰度很低,作为中度不相容元素,简单的岩浆形成、演化过程很难使之从地壳丰度直接富集到工业品位。我们研究结果显示钼的成矿主要通过两阶段富集过程来实现:一是与风化、沉积有关的表生过程;二是与板块俯冲或深埋熔融有关的岩浆过程。钼是变价元素,在寒武纪大气氧再次升高以后,钼在地表化学风化过程中容易被氧化为水溶性的Mo O42-,进入地表径流和海洋湖泊中,并且在还原条件下进入富含有机质的黑色页岩等沉积物(岩)中。富钼沉积物(岩)在随板块俯冲到地幔或深埋等条件下可以因升温变质,进而发生部分熔融,形成富钼的原始岩浆,在俯冲条件下往往形成斑岩铜(金)钼矿床,氧逸度低于斑岩铜矿,而斑岩钼矿的氧逸度更低。具有高化学风化速率、大的流域面积的封闭、半封闭型水域和河口地区是表生过程中钼富集的最佳区域,是大型钼矿形成的基础。
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| 关 键 词： | 钼 钼矿 化学风化 富钼沉积物 氧逸度 |
| 收稿时间： | 2014/9/22 0:00:00 |
| 修稿时间： | 2015/2/15 0:00:00 |
The geochemical behavior of molybdnum and mineralization. |
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| SUN WeiDong,LI CongYing,LING MingXing,DING Xing,YANG XiaoYong,LIANG HuaYing,ZHANG Hong and FAN WeiMing.The geochemical behavior of molybdnum and mineralization.[J].Acta Petrologica Sinica,2015,31(7):1807-1817. |
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| Authors: | SUN WeiDong LI CongYing LING MingXing DING Xing YANG XiaoYong LIANG HuaYing ZHANG Hong and FAN WeiMing |
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| Institution: | CAS Key Laboratory of Mineralogy and Metallogeny, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China;CAS Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, Beijing 100101, China,CAS Key Laboratory of Mineralogy and Metallogeny, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China,State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China,State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China,School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026 China,CAS Key Laboratory of Mineralogy and Metallogeny, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China,Department of Geology, Northwest University, Xi'an 710069, China and CAS Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, Beijing 100101, China |
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| Abstract: | Molybdenum is a rare element with very low abundance in the silicate Earth. It is a moderately incompatible element. Therefore, Mo cannot be enriched to minable grade through simple magmatism processes. Our studies show that one of the most important ways that enriches Mo is oxidation and reduction during chemical weathering. Molybdenum can be easily oxidized to form water solvable MoO42- in surface environment, especially after the second major elevation of atmospheric oxygen at ~550Myr ago, transported to oceans and lakes, and then retained by anoxic sediments, in the form of thio molybdates. Subsequent partial melting of metamorphosed Mo enriched sediments further enriches Mo, which may form Mo-rich magmas. Porphyry-Cu-Mo deposits in the American continents in the East Pacific is accompanied by slab melting. Direct partial melting of high grade metamorphosed Mo-rich sediments may form pure Mo porphyry with slightly lower oxygen fugacities. High chemical weathering rates, large catchment areas and closed or semi-closed water bodies are favorable places for Mo enrichment, which may form large Mo ore fields through later events. |
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| Keywords: | Molybdenum Mo ore Chemical weathering Mo-rich sediments Oxygen fugacity |
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