中国锑矿成矿规律概要
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国家自然科学基金项目(面上项目,重点项目,重大项目)


Summary of Metallogenic Regularities of Antimony Deposits in China
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    摘要:

    锑是中国的优势矿种之一。本文在全国矿产资源潜力评价项目的基础上,对中国锑矿床的成矿地质背景、赋矿围岩、控矿构造和成矿时代等进行了综合分析,简要总结了中国锑床的分布特征与成矿规律,同时提出了一些科学问题。中国锑矿床类型多,主要形成于中生代和新生代,而显生宙前则未有锑矿形成,集中分布在西南天山、小兴安岭-张广才岭、昆仑-秦岭、长江中下游、藏北、藏南、西南三江、滇黔桂、江南隆起、湘中-桂中北、南岭、东南沿海等12个成锑带。当前需要从区域尺度来探讨锑矿床的形成机制,加强成矿规律和成矿系列的研究,以理论指导锑矿资源的再发现.

    Abstract:

    Antimony is one of the dominant minerals in China. In this paper, based on the mineral resource potential assessment project, the authors clarifies the distribution characteristics and metallogenic of antimony deposits through comprehensive analysis of some features, including geological background of ore-formation, ore-hosting rocks, ore-controlling structures and metallogenetic epochs of the antimony deposits in China, and put forward some scientific problems. Antimony deposits in China consist of various types, and were formed in Phanerozoic, mainly in the Mesozoic and the Cenozoic, and concentrated in Southwestern Tianshan antimony belt, Xiaoxing’anling-Zhangguangcailing antimony belt, Kunlun-Qinling antimony belt, the middle-lower Yangtze antimony belt, Northern Tibet antimony belt, Southern Tibet antimony belt, Southwestern Sanjiang antimony belt, Yunnan-Guizhou-Guangxi antimony belt, Jiangnan uplift antimony belt, Central Hunan-Northern Guangxi antimony belt, Nanling antimony belt and southeast coast antimony belt. We need to study the metallogenetic mechanism of antimony deposits from the regional scale, especially on the metallogenic regularity and metallogenic series, guiding the discovery of new antimy deposits.

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王永磊,徐珏,张长青,王成辉,陈郑辉,黄凡.2014.中国锑矿成矿规律概要[J].地质学报,88(12):2208-2215.
WANG Yonglei, XU Jue, ZHANG Changqing, WANG Chenghui, CHEN Zhenghui, HUANG Fan.2014. Summary of Metallogenic Regularities of Antimony Deposits in China[J]. Acta Geologica Sinica,88(12):2208-2215.

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  • 收稿日期:2014-08-31
  • 最后修改日期:2014-11-21
  • 录用日期:2014-12-03
  • 在线发布日期: 2014-12-09
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