内生热液成矿理论越来越多地基于定量的物理化学因素,因而在有关的研究中,通常把很多的注意力集中在矿质来源及其沉积机制上。在这两个方面,许多科学家收集了综合性资料,结果表明,矿质来源具多成因性,同时在地球化学临界值内导致成矿物质局部富集的特定因素也是多种多样的。在不同时代,不同 Endogenic hydrothermal mineralization theories are increasingly based on quantitative physico-chemical factors, so much attention has often been focused on mineral sources and deposition mechanisms in related studies. In both cases, many scientists have collected comprehensive data that show that there are many genetic causes of mineral sources, and there are also many specific factors that cause local enrichment of metallogenic materials within geochemical thresholds. In different times, different