现代海底热液化学组成特征及其控制因素
The chemical characteristics and their controlling factors of seafloor hydrothermal fluids
查看参考文献32篇
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文摘
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1948年瑞典科学家利用"信天翁号"(Albatross)科学考察船在红海中部的Atlantis Ⅱ深渊附近发现了高温高盐溶液,第一次揭示了海底热液活动的存在。1979年在21°N东太平洋海隆(EPR)地区发现了高达10余米的金属硫化物烟囱并首次采集到了温度高达350~400℃的热液[1]。随后,在不同速率的扩张洋脊和大洋板块中都发现了数目众多的热液活动区。迄今为止,在全球洋底已经发现了200多个热液喷口,500多个热液硫化物矿藏区~([2])。 |
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来源
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海洋科学
,2010,34(4):95-99 【核心库】
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关键词
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热液
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海底
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化学
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地址
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1.
武汉理工大学资源与环境工程学院, 湖北, 武汉, 430070
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中国科学院广州地球化学研究所, 海洋地质国家重点实验室, 广东, 广州, 510640
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中国科学院广州地球化学研究所, 广东, 广州, 510640
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语种
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中文 |
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文献类型
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综述型 |
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ISSN
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1000-3096 |
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学科
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海洋学 |
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基金
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中国博士后科学基金
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国家自然科学基金重点项目
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文献收藏号
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CSCD:3903923
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32
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