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首页> 外文期刊>Doklady Earth Sciences >Ferromanganese Crusts of the Doldrums Fracture Zone, Central Atlantic: New Data on the Chemical Composition
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Ferromanganese Crusts of the Doldrums Fracture Zone, Central Atlantic: New Data on the Chemical Composition

机译:中央大西洋中央大西洋骨折区的铁锰裂纹:化学成分的新数据

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摘要

New data on the morphology, chemical composition, and age of the ferromanganese crusts of the Doldrums Fracture Zone, Central Atlantic, collected during the 45th cruise of the R/V Akademik Nikolai Strakhov, are presented. According to studies of the chemical composition, the Doldrums crusts are characterized by high concentrations of Fe, Al, Si, and trace elements-Cd, Cr, Li, Hf, Nb, Sb, Sc, Th, W, and V. Most of the crusts have a two-layer structure: the upper layer shows an increased content of detritus and lower concentrations of Mn, Fe, Co, Ni, Cu, and REEs in comparison with the lower layer. The two-layered structure reflects the change in the conditions of crust formation.
机译:展示了关于r / v Akademik Nikolai Strakhov的45次巡航中,大西洋中央大西洋中央大西洋中央大西洋的形态学,化学成分和年龄的新数据。 根据化学成分的研究,低玻璃状外壳的特征在于高浓度的Fe,Al,Si和痕量元素-CC,Cr,Li,HF,Nb,Sb,Sc,Th,W和V.大部分 结壳具有双层结构:上层显示与下层相比,上层显示滴乳含量和较低浓度的Mn,Fe,Co,Ni,Cu和REES。 双层结构反映了地壳形成条件的变化。

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