Science. 1967 Jul 7;157(3784):63-5. doi: 10.1126/science.157.3784.63.
Mineralogical and chemical analyses performed on 67 ferromanganese nodules from widely varying locations and depths within the marine environment indicate that the minor element composition is controlled by the mineralogy, and that the formation of the mineral phases is depth dependent.
对来自海洋环境中不同位置和深度的 67 个铁锰结核进行的矿物学和化学分析表明,微量元素组成受矿物学控制,并且矿物相的形成是深度相关的。