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

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

朱金初

南京大学地球科学系和成矿作用国家重点实验室，南京 210093

收稿日期:2003-12-20 修回日期:2003-12-20 出版日期:2003-12-20 发布日期:2003-12-20

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

Zhu Jin-chu

Department of Earth Sciences and Key State Laboratory for Mineral Deposits Research, Nanjing University, Nanjing 210093

Received:2003-12-20 Revised:2003-12-20 Online:2003-12-20 Published:2003-12-20

摘要/Abstract

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一热液叠加成因机制，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。

Abstract: 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 sedimentation-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 Department 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 domestic investigators and supported by geological exploration practice．

朱金初. 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[J]. J4.

Zhu Jin-chu. A Brief Review for the Study on Genesis of the Submarine Volcanic Exhalative Sedimentary Deposits in South China[J]. J4.