| 广东乐昌杨柳塘铅锌矿床成矿作用分析 |
| |
| 引用本文： | 王增润,陈子龙. 广东乐昌杨柳塘铅锌矿床成矿作用分析[J]. 中南大学学报(自然科学版), 1986, 0(6) |
| |
| 作者姓名： | 王增润 陈子龙 |
| |
| 作者单位： | 中南矿冶学院地质系，中南矿冶学院地质系 |
| |
| 摘 要： | 作者通过野外及室内综合研究,对该矿床地质地球化学特征、成矿物质来源、成矿作用过程及成矿作用方式等问题进行了较全面的探讨,以较充分的证据说明该矿床属海相沉积(可能含部分远源海底火山喷发沉积)-地下热卤水改造成因的层控型矿床。文中并指出了找矿方向。
|
| 关 键 词： | 海相沉积 地下热卤水 矿源层 层控型矿床 |
AN ANALYSIS OF THE MINERALIZATION OF THE LEAD-ZINC ORE DEPOSITS IN YANGLIUTANG,LECHANG,GUANGDONG |
| |
| Wang Zengran,Chen Zilong. AN ANALYSIS OF THE MINERALIZATION OF THE LEAD-ZINC ORE DEPOSITS IN YANGLIUTANG,LECHANG,GUANGDONG[J]. Journal of Central South University:Science and Technology, 1986, 0(6) |
| |
| Authors: | Wang Zengran Chen Zilong |
| |
| Affiliation: | Wang Zengran;Chen Zilong Department of Geology |
| |
| Abstract: | The origin of the lead-zinc ore deposits in Yangliutang of Guangdong is similiar to that of the Fankou lead-zinc ore deposits in Guangdong.The features of geochemistry,the resourses of the ore-forming material,the processcs and depositional types of the mineralization of the ore deposits are studied and determined.A lot ofevidence indicate that the ore deposits may be referred to the strata-bound ore deposits which were formed by submarine sedimentation(probably partly volcanic sedimentation of far-off resourses)and the reformation of underground hot saline brine.The directions in researching for new ore deposits in this area are also suggested in this paper. |
| |
| Keywords: | Submarine sedimentation Underground hot saline brine Source-bed Strata-bound ore deposit |
| 本文献已被 CNKI 等数据库收录！ |
|
