CAJ | 학술논문

表生地球化学酸碱性风化，对矿体氧化露头成矿元素的滞留或流失、分散或次生富集具有明显的控制作用。本文讨论在不同的酸碱性风化条件下，成矿元素按其本身的地球化学性状，另行组成适合表生环境的稳定化合物或矿物，进行元素再分配。利用成矿元素的地化性状，对元素表生地化行迹顺向追踪其次生富集，逆向追踪原生矿的矿物组合和元素组合，从中提炼找矿信息，指示找矿评价工作。
표생지구화학산감성풍화，대광체양화로두성광원소적체류혹류실、분산혹차생부집구유명현적공제작용。본문토론재불동적산감성풍화조건하，성광원소안기본신적지구화학성상，령행조성괄합표생배경적은정화합물혹광물，진행원소재분배。이용성광원소적지화성상，대원소표생지화행적순향추종기차생부집，역향추종원생광적광물조합화원소조합，종중제련조광신식，지시조광평개공작。
Dispersion and enrichment of chemical elements from an ore outcrop are controlled by weathering. This paper makes an approach to the control of weathering under different pH conditions over redistribution and secondary enrichment of elements from exposed ores in order to obtain prospecting information.