|
|||||
|
|
| 云南个旧锡矿床铅、硫同位素研究 | |
| 引用本文： | 黎应书,秦德先,党玉涛,薛传东,谈树成,陈爱兵,贾国相. 云南个旧锡矿床铅、硫同位素研究[J]. 地质与勘探, 2006, 42(2): 49-53 |
| 作者姓名： | 黎应书 秦德先 党玉涛 薛传东 谈树成 陈爱兵 贾国相 |
| 作者单位： | 昆明理工大学矿产地质研究所,昆明,650093;云南锡业集团公司,个旧,661000;云南大学资源环境与地球科学学院,昆明,650091;桂林矿产地质研究院,桂林,541004 |
| 基金项目： | 科技部专项基金，云南省自然科学基金 |
| 摘 要： | 对个旧锡矿床的铅、硫同位素进行了研究,研究结果表明,矿石中的铅、硫同位素主要来自基性岩,少量来自花岗岩,矿床的形成经历了印支期的基性火山成矿作用(铅模式年龄200-280Ma)和燕山期花岗岩的叠加改造成矿作用(铅模式年龄80-160Ma).进一步表明,个旧锡矿床为一个多成因多物质来源的矿床. |
| 关 键 词： | 锡矿床 铅同位素 硫同位素 云南个旧 |
| 文章编号： | 0495-5331(2006)02-0049-05 |
| 收稿时间： | 2005-01-11 |
| 修稿时间： | 2005-03-23 |
LEAD AND SULPHUR ISOTOPE OF GEJIU TIN DEPOSIT IN YUNNAN PROVINCE |
|
| LI Ying-shu,QIN De-xian,DANG Yu-tao,XUE Chuan-dong,TAN Shu-cheng,CHEN Ai-bing,JIA Guo-xiang. LEAD AND SULPHUR ISOTOPE OF GEJIU TIN DEPOSIT IN YUNNAN PROVINCE[J]. Geology and Prospecting, 2006, 42(2): 49-53 | |
| Authors: | LI Ying-shu QIN De-xian DANG Yu-tao XUE Chuan-dong TAN Shu-cheng CHEN Ai-bing JIA Guo-xiang |
| Affiliation: | 1. Geological Institute of Mineral Deposits, Kunming University of Science and Technology, Kunming 650093 ; 2. Yunnan Tin Corporation, Gejiu 661000;3. School of Resources, Environment and Earth Sciences, Yunnan University, Kunming 650091 ;4. Guilin Institute of Geology for Mineral Resources, Guilin 541004 |
| Abstract: | Lead and sulphur isotopes of Gejiu tin deposit have been studied.The results show that lead and sulphur isotopes in ores came mostly from basic rocks while some came from granite.Formation of the deposit underwent Indo-Sinian basic volcanic mineralization(mode age of lead isotope from 200 to 280 Ma) and Yanshanian granitic superimposition mineralization(mode age of lead isotope from 80 to 160 Ma).It is further proved that Gejiu tin deposit is a compound genesis type. |
| Keywords: | tin ore deposit lead isotope sulphur isotope Gejiu Yunnan province |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ | |
| 点击此处可从《地质与勘探》浏览原始摘要信息 | |
| 点击此处可从《地质与勘探》下载全文 | |