Integrated with other features of the deposit, it is thought that microorganism plays an important role in the natural oxidization enrichment process of manganese.
实验结果表明这两种细菌对锰具有明显的氧化作用,结合矿床的其他方面特征,认为自然界中微生物在锰的氧化富集过程中起着积极的作用,作用表现在两个方面:一方面微生物可以直接对锰进行氧化,使原生碳酸锰矿转变为氧化锰矿;另一方面微生物又可以改变环境的pH值,促进锰的化学氧化。
Finally,combined with studies on the limit of regional ore-bearing depth and the ore body spatial location model,it was predicted that a second mineralization enrichment zone might exist beneath Ⅳ and Ⅶ ore bodies along SW side dipping direction.
结合区域含矿下限的分析和矿体空间产状模式,推断Ⅳ和Ⅶ号矿体沿SW侧伏方向向下可能出现第二矿化富集带。
It was discovered in the oxidation zone of Tl-rich ore bodies, Lanmuchang Tl (Hg) deposit, Xinren County, Guizhou Province and is associated with melanterite, pickeringite, potassium alum, jarosite, gypsum, arsenic blane, sulphur and some unknown minerals.
铊明矾 (lanmuchangite ,TlAl[SO4]2 ·12H2 O)是在贵州滥木厂铊 (汞 )矿床富铊矿体氧化带中发现的一种铊的硫酸盐新矿物。
