吸附作用被认为是低温表生矿床的一种重要的成矿机制。

Adsorption is regarded as an important metallogenic mechanism for the supergene and epithermal ore deposits.

youdao

湖润锰矿床由海相沉积的原生碳酸锰矿床和表生富集的氧化锰矿床组成。

Hurun manganese deposit is consisted of Marine sedimentary primary manganese carbonate ores and supergene enrichment oxide ores.

youdao

认为表生富集型氧化锰矿床的形成主要受原生含锰层、地质构造、地形地貌、顶盖层厚度、岩性、气候及水文地质等条件所制约。

Formation of the oxidized Mn deposit is controled by the primary Mn ore layer, tectonics, geomorphology, thickness and lithology of the cover rock, climate and hydrogeological condition.

youdao