干旱气候变化与可持续发展

生物成矿作用和超大型矿床的成因

  • 周涛发 ,
  • 范裕 ,
  • 袁峰 ,
  • 张鑫
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  • 中国科学院地质研究所
李任伟

收稿日期: 1989-12-05

  网络出版日期: 1990-05-01

摘要

以元古代南非威特沃特斯兰德含金砾岩型金矿床和元古代燧石条带含铁建造的研究为例阐述了生物成矿作用和超大型沉积矿床成因之间的密切联系。生物作用是地球表层最活跃和强大的地质营力,对沉积岩石圈内超大型矿床的形成和改造具有重大的影响。

本文引用格式

周涛发 , 范裕 , 袁峰 , 张鑫 . 生物成矿作用和超大型矿床的成因[J]. 地球科学进展, 1990 , 5(3) : 8 -11 . DOI: 10.11867/j.issn.1001-8166.1990.03.0008

参考文献

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