浅谈热水沉积矿床地质地球化学研究进展与趋势  

The Research Progress and Trends on Geology and Geochemical of Hydrothermal Sedimentary Deposit

作　　者：周闻达[1] 叶锡芳[2] 

机构地区：[1]中国地质大学,武汉430074 [2]浙江省第三地质大队,金华321001

出　　处：《科技通报》2014年第1期31-38,共8页Bulletin of Science and Technology

摘　　要：热水沉积成矿作用是近代成矿理论的重大发现,热水沉积的矿床有着规模大,品位高的特点。本文依据前人研究成果,阐述了热水沉积矿床地质地球化学研究进展,存在问题与发展趋势。The hydrothermal mineralization is an important discovery of modern metallogenic theory. Hydrothermal sedimentary deposits have great size and high grade features. This paper based on the results of previous studies,reviews the geochemical research progress, problems and trends of the hydrothermal sedimentary deposit on the basis of Chinese and foreign literature published recently.

关 键 词：热水沉积作用 热水沉积矿床 研究进展与趋势 

分 类 号：P58[天文地球—岩石学]