菱铁矿
元古代
地质学
带状铁形成
磁异常
地球化学
转化(遗传学)
异常(物理)
矿物学
前寒武纪
古生物学
化学
黄铁矿
生物化学
构造学
物理
凝聚态物理
基因
作者
M. M. Astafieva,Л. В. Зайцева
标识
DOI:10.1134/s0031030120080031
摘要
Interesting observations illustrating the process of transformation of some minerals of banded iron formations (BIF) were made while studying the Early Proterozoic jaspilites of the Kursk Magnetic Anomaly (KMA). Examples showing the process of siderite transformation into iron oxides/hydroxides by iron-oxidizing bacteria are given.
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