on the denudation surfaces with varying elevation, the difference among weathering profiles is result of different laterization processes.
在不同海拔高度的山前剥蚀面上,风化壳红土化程度的差异,是不同时期风化作用的产物。
the well developed weathering crust often presents three-layer structure, gold is primarily concentrated in the middle-upper part where the laterization is relatively intensive.
发育完好的红土型风化壳常呈现三层结构,金主要富集在红土化较强烈的中上部。
in the humid-warm climatic conditions, the laterization can cause gold to be migrated and reconcentrated in weathering crust.
在湿热的气候条件下,红土化作用可使金在风化壳中迁移再富集。
supergenous enrichment of gold during the laterization is also discussed.