| 华南锑矿带的成矿时代和成矿构造环境 |
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| 引用本文： | 彭建堂,胡瑞忠.华南锑矿带的成矿时代和成矿构造环境[J].地球与环境,2001,29(3):104-108. |
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| 作者姓名： | 彭建堂 胡瑞忠 |
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| 作者单位： | 中国科学院地球化学研究所, |
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| 基金项目： | 国家攀登计划预选项目 (编号 :95 预 2 5 )，中科院矿床地球化学开放实验室创新基金 |
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| 摘 要： | 在收集整理已有的同位素定年数据的基础上 ,应用构造 -岩浆活化理论分析了华南锑矿带的成矿时代和成矿构造环境。研究表明 ,华南锑矿带存在多期次的成矿作用 ,最早为加里东晚期 ,最晚为喜山期 ;但大规模、爆发性的成矿作用为晚燕山期 ,大约在 1 0 0Ma左右 ;华南锑矿带大规模成矿的构造环境为自治活化区构造 -岩浆活化的第二阶段
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| 关 键 词： | 成矿时代 成矿构造环境 锑矿带 华南 |
| 文章编号： | 1008-0244(2001)03-0104-05 |
| 修稿时间： | 2001年4月26日 |
METALLOGENIC EPOCH AND METALLOGENIC TECTONIC ENVIRONMENT OF ANTIMONY DEPOSITS, SOUTH CHINA |
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| Peng Jiantang,Hu Ruizhong.METALLOGENIC EPOCH AND METALLOGENIC TECTONIC ENVIRONMENT OF ANTIMONY DEPOSITS, SOUTH CHINA[J].Earth and Environment,2001,29(3):104-108. |
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| Authors: | Peng Jiantang Hu Ruizhong |
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| Abstract: | Based on the isotope dates available for antimony deposits, South China, the authors, guided by the theory of tectonic-magmatic activation, preliminarily studied the metallogenic epoch and metallogenic tectonic background of the Sb ore belt, South China. It was revealed that there existed multi-stage Sb mineralization in South China, the earliest Sb mineralization took place during the Caledonian period, and the latest mineralization happened during the Himalayanian period. However, the large-scale Sb mineralization in this area was restricted within Late Yenshanian at about 100Ma ago. The metallogenic tectonic background of large-scale Sb mineralization in South China is the second stage of tectonic-magmatic activation in the self-activated zone. |
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| Keywords: | metallogenic epoch metallogenic tectonic environment antimony deposit South China |
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