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| 黑龙江老柞山金多金属矿床地质地球化学初探 | |
| 引用本文： | 代立东,李和平,王思源,魏俊浩.黑龙江老柞山金多金属矿床地质地球化学初探[J].地球与环境,2002,30(2):19-24. |
| 作者姓名： | 代立东 李和平 王思源 魏俊浩 |
| 作者单位： | 1. 中国科学院地球化学研究所,贵州,贵阳,550002 2. 中国地质大学,湖北,武汉,430074 3. 中国科学院地球化学研究所,贵州,贵阳,550002;中国地质大学,湖北,武汉,430074 |
| 基金项目： | 国家科技部攀登计划预选项目 (95 预 3 9)，中国科学院“百人计划” |
| 摘 要： | 通过对老柞山金多金属矿床地质背景、硫同位素、铅同位素、碳氧同位素以及包裹体和岩石化学的研究 ,得出产金矿带成矿热液为高温岩浆热液 ,并有地壳物质混入 ,该矿床形成于活动大陆边缘钙碱系列环境。 |
| 关 键 词： | 金多金属矿床 硫同位素 铅同位素 碳氧同位素 包裹体 岩石化学 老柞山 |
| 文章编号： | 1008-0244(2002)02-0019-06 |
| 修稿时间： | 2001年9月10日 |
GEOLOGY AND GEOCHEMISTRY OF LAOZUOSHAN GOLD-POLYMETAL ORE DEPOSIT IN HEILONGJIANG PROVINCE |
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| Dai Lidong ,Li Heping ,Wang Siyuan ,Wei Junhao.GEOLOGY AND GEOCHEMISTRY OF LAOZUOSHAN GOLD-POLYMETAL ORE DEPOSIT IN HEILONGJIANG PROVINCE[J].Earth and Environment,2002,30(2):19-24. | |
| Authors: | Dai Lidong Li Heping Wang Siyuan Wei Junhao |
| Institution: | Dai Lidong 1,Li Heping 1,Wang Siyuan 2,Wei Junhao 1,2 |
| Abstract: | In this paper, through the study of ore deposit geologic settings, sulphur isotopes, lead isotopes, carbon isotopes, oxygen isotopes, fluid inclusions and petrochemistry, the authors have drawn a conclusion that gold ore deposits were derived from high temperature magmatic hydrothermal solutions with underground water involved. It is the first time that the authors put forward that the Laozuoshan gold polymetal ore deposit in Heilongjiang Province was formed in a calc alkaline environment at the continental margin. |
| Keywords: | gold polymetal ore deposit sulphur isotope lead isotope carbon isotope oxygen isotope inclusion petrochemistry Laozuoshan |
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