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元素共生分异现象在矿床中是普遍存在的。认识和查明元素的共生分异特征和形成机制 ,对丰富成矿理论和指导找矿勘探均具有重要意义。以黔西南微细浸染型金矿区为例 ,对元素共生分异机制的研究现状和存在问题进行了评述。在此基础上 ,肯定了成矿流体地球化学在元素共生分异机制研究中的地位和作用。从成矿流体地球化学研究入手 ,在查明成矿流体来源及时空演化规律的基础上 ,结合矿床地球化学、成矿实验及成矿过程的计算机模拟研究 ,深入研究成矿流体中成矿元素的来源、活化迁移条件及沉淀富集过程的共性及差异 ,是揭示元素共生分异机制的关键所在
The phenomenon of elemental symbiosis is ubiquitous in the deposit. Understanding and identifying elements of the symbiotic differentiation characteristics and formation mechanism for the rich mineralization theory and guidance of prospecting exploration are of great significance. Taking the finely disseminated gold mine in southwestern Guizhou Province as an example, the current situation and existing problems of the symbiotic differentiation mechanism of elements were reviewed. On this basis, the position and function of geochemistry of ore-forming fluids in the study of symbiosis mechanism of elements were affirmed. Based on the geochemical study of ore-forming fluid, based on the study of source of fluid and temporal and spatial evolution of ore-forming fluid, combined with the geochemical and ore-forming experiments of mineral deposits and the computer simulation of metallogenic process, The origin, activation and migration conditions, and the commonness and difference of precipitation enrichment process are the keys to reveal the mechanism of elemental symbiosis