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华南陆块陆内成矿作用的一些科学问题
Some scientific questions on the intra-continental metallogeny in the South China continent

查看参考文献119篇

胡瑞忠 1   毛景文 2   范蔚茗 3   华仁民 4   毕献武 1   钟宏 1   宋谢炎 1   陶琰 1  
文摘 华南陆块由扬子地块和华夏地块组成,是全球罕见的世界级多金属成矿省,成矿潜力巨大.华南陆块的形成和演化,受到了很有特色的陆内大陆动力学过程的影响,其中的晚古生代地幔柱成矿系统、中生代大面积低温成矿系统、中生代大花岗岩省成矿系统等陆内成矿系统,在全球背景中很有特色,是全球研究陆内成矿作用的理想基地.对华南陆块地质历史时期的大陆动力学过程如何制约上述成矿作用的发生,以往已开展不同程度的研究并取得重要成果.笔者在论述这些研究进展的基础上,提出了三大成矿系统需要进一步研究的一些科学问题.
其他语种文摘 The South China continent including the Yangtze Block and the Cathaysia Block is an uncommon world-class polymetallic metallogenic province with great ore-forming potential. The formation and evolution of the South China continent had undergone specific intra-continental dynamic processes, in which the Late Permian plume-related metallogenic system, the Mesozoic huge low-temperature metallogenic system and the metallogenic system of the Mesozoic great granite province are quite distinctive in the world. Thus, the South China continent becomes an ideal international base for studying the intra-continental mineralization. The studies, in various levels, of how the continental dynamic processes over different geological time control the mineralization in the South China continent have been carried out and have had important achievements. On the basis of these studies, this paper presents the major scientific questions for further research on the three metallogenic systems.
来源 地学前缘 ,2010,17(2):13-26 【核心库】
关键词 华南陆块 ; 陆内成矿作用 ; 地幔柱成矿系统 ; 大面积低温成矿系统 ; 大花岗岩省成矿系统
地址

1. 中国科学院地球化学研究所, 矿床地球化学国家重点实验室, 贵州, 贵阳, 550002  

2. 中国地质科学院矿产资源研究所, 北京, 100037  

3. 中国科学院广州地球化学研究所, 广东, 广州, 510640  

4. 南京大学地球科学系, 江苏, 南京, 210093

语种 中文
文献类型 研究性论文
ISSN 1005-2321
学科 地质学
基金 国家973计划 ;  国家自然科学基金重点项目
文献收藏号 CSCD:3856262

参考文献 共 119 共6页

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