华南海相火山喷流沉积矿床成因研究简评——兼述徐克勤教授在该领域的重大贡献  

A Brief Review for the Study on Genesis of the Submarine Volcanic Exhalative Sedimentary Deposits in South China

作　　者：朱金初[1] 

机构地区：[1]南京大学地球科学系和成矿作用国家重点实验室,南京210093

出　　处：《高校地质学报》2003年第4期536-544,共9页Geological Journal of China Universities

基　　金：国家自然科学基金(编号:40073008;40132010)

摘　　要：在华南地区,发育着大量层状和层控铜、铅、锌、铁、金、银、锡、硫等矿产资源,20世纪70年代以前,一般都认为这些矿床是热液或矽卡岩成因。徐克勤教授在70年代中期提出了断裂拗陷带构造背景条件下的火山喷流沉积-热液叠加成因机制,并在嗣后长久的岁月中,带领南京大学师生进行了大量的研究工作,取得了丰富的研究成果。这一成因认识,已经在国内科研人员中获得广泛的认同,并被大量地质找矿实践所支持。Many stratiform and stratabound Cu, Pb, Zn, Fe, Au, Ag, Sn, S mineral deposits are found in South China. They were interpreted as hydrothermal or skarn type in origin up to early 1970's. In middle 1970's Professor Xu Keqin proposed a submarine volcanic exhalative sedimen- tation- hydrothermal superimposition origin for these mineral deposits, specifically formed in the fault depression environment. Led by Prof. Xu, the academic staff and students in the Depart- ment of Earth Sciences, Nanjing University conducted a large amount of investigations in this field and gained significant achievements. Nowadays this point of view is recognized by most do- mestic investigators and supported by geological exploration practice.

关 键 词：华南 矿产资源 断裂拗陷带 火山喷流沉积 热液叠加 

分 类 号：P618.4[天文地球—矿床学]