Doklady Earth Sciences ( IF 0.9 ) Pub Date : 2021-09-07 , DOI: 10.1134/s1028334x21080092 G. V. Novikov 1 , L. I. Lobkovsky 1 , N. V. Lobus 1 , O. Yu. Bogdanova 1 , T. Eu. Sedysheva 2, 3
Abstract
The main ore minerals of all layers of cobalt-rich ferromanganese crusts of Guyot Govorov of the Magellanic Mountains of the Pacific Ocean are poorly crystallized, poorly structurally ordered Fe-vernadite, Mn-feroxigite. A sufficiently structurally ordered vernadite, which is mainly found in layer I–1 and in a smaller amount in layer I–2, has also been identified as goethite. As an impurity, asbolan-buzerite and buzerite-I are noted. The distribution of cations of non-ferrous, heavy, rare, and rare-earth elements in the layers of Govorov Guyot crusts indicates that they are clearly unevenly supplied to the cobalt-rich ferromanganese crusts.
中文翻译:
太平洋麦哲伦山脉Govorov Guyot富钴铁锰结壳的矿石含量
摘要
太平洋麦哲伦山脉Guyot Govorov各层富钴铁锰结壳的主要矿石矿物为结晶性差、结构有序性差的Fe-vernadite、Mn-feroxitite。一种结构足够有序的vernadite,主要存在于I-1 层,少量存在于I-2 层,也被确定为针铁矿。作为杂质,注意到asbolan-buzerite和buzerite-I。有色金属、重元素、稀有元素和稀土元素在 Govorov Guyot 地壳各层中的分布表明它们明显不均匀地供给富钴铁锰地壳。