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马尔库斯海脊富钴结壳的钙质超微化石生物地层学研究

马维林 金翔龙 钟石兰 初凤友

马维林, 金翔龙, 钟石兰, 初凤友. 马尔库斯海脊富钴结壳的钙质超微化石生物地层学研究[J]. 海洋学报, 2007, 29(5): 174-180.
引用本文: 马维林, 金翔龙, 钟石兰, 初凤友. 马尔库斯海脊富钴结壳的钙质超微化石生物地层学研究[J]. 海洋学报, 2007, 29(5): 174-180.
MA Wei-lin, JIN Xiang-long, ZHONG Shi-lan, CHU Feng-you. Calcareous nannofossil biostratigraphy study of cobalt-rich crust from Marcus Sea Ridge[J]. Haiyang Xuebao, 2007, 29(5): 174-180.
Citation: MA Wei-lin, JIN Xiang-long, ZHONG Shi-lan, CHU Feng-you. Calcareous nannofossil biostratigraphy study of cobalt-rich crust from Marcus Sea Ridge[J]. Haiyang Xuebao, 2007, 29(5): 174-180.

马尔库斯海脊富钴结壳的钙质超微化石生物地层学研究

基金项目: 中国大洋矿产资源研究开发协会“十五”专项基金资助项目(DY105-01-01-01)

Calcareous nannofossil biostratigraphy study of cobalt-rich crust from Marcus Sea Ridge

  • 摘要: 分布于大洋盆地高地形区的富钴结壳是一种经历了上千万年生长历程的、含多种有价值金属的特殊“沉积物”.与一般沉积物一样,富钴结壳也保存了海洋环境变迁更替的信息.正确解读结壳的生长历史,不仅对认识这种有用金属矿产的成因和成矿机制有重要意义,而且对研究第三纪以来的大洋古环境乃至这一时段的全球环境变化也有不容忽视的价值.
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出版历程
  • 收稿日期:  2005-12-27
  • 修回日期:  2006-12-04

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