海底热液活动研究综述  

SUMMARIZING ON THE STUDY OF HYDROTHERMAL ACTIVITIES ON THE SEAFLOOR

作　　者：高爱国[1] 

机构地区：[1]中国科学院海洋研究所

出　　处：《海洋地质与第四纪地质》1996年第1期103-110,共8页Marine Geology & Quaternary Geology

基　　金：国家自然科学基金

摘　　要：本文简要介绍海底热液活动的研究历史以及目前的研究状况，同时谈了作者对海底热液活动研究的一些认识。It is great event in the oceanology this century that hydrothermal activities andhydatogeneses are discovered on seabed.We have now had much knowkdge of hy-drothermal activities under different geologic settings,and mastered some symbols andmeans to find them after more than 30 years'study.At least there are a hundred hy-drothermal activity areas on seabeds of the world,in which many ore-grade depositsexsit.In-situ observation and laboratory analysis and simulation have provided more op-portunities for us to understand material source of hydrothermal activities,condition ofmineral formation and exchanges of materials on seabed interfaces. 16 main events andthe present situation on the studies of hydrothermal activities have been introduced inthis paper.Conclusion is that sources of material to deposits are abundant because thematerial sources of hydrothermal deposits on seabeds are dominantly halogen-rich sea-water which makes up most of the hydrothermal solution,trace element-rich seafloorsediments and magmatic activities.It is possible that the hydrothermal deposits becomean important kind of mineral resources because they are easy to be found, mined andsmelted compared with ferromanganese crusts.To find more hydrothermal deposits onseabed,studies on magmatism,tectonism,water depth and other conditions which con- trol the hydrothermal activities must be strengthened.

关 键 词：海底 热液活动 热液成矿 热液矿床 

分 类 号：P611.1[天文地球—矿床学] P736.3[天文地球—地质学]