喷流沉积成矿作用研究的若干问题  

SOME PROBLEMS IN STUDIES OF THE EXHALATIVE SEDIMENTARY MINERALIZATION

作　　者：刘继顺[1] 

机构地区：[1]中南工业大学地质系

出　　处：《矿产与地质》1996年第1期6-10,共5页Mineral Resources and Geology

摘　　要：研究海底喷流沉积矿床形成和陆源沉积速率，可确定喷流沉积矿床处于上盘蚀变的找矿标志和块状硫化物矿床产出的海底深度。此外还探讨了陆相喷流沉积成矿的可能性。The rate of terrigenous sedimentation which constrains the formation and preservation of the submarne exhalative sedimentary deposits can be considered as an indicator to prospect for the exhalative sedimentary deposits in the hanging-wall alteration and can determine the submarine depth at which massive sulfide deposits occur. In addition, the possibity of the continental exhalative sedimentary minerlization is also discussed in this paper.

关 键 词：喷流沉积 成矿作用 沉积矿床 

分 类 号：P612[天文地球—矿床学]