辽宁省重点金矿集区地质特征及成岩成矿作用

袁和1, 白银增2, 耿树峰1, 洪秀伟1, 王登红3. 2023. 辽宁省重点金矿集区地质特征及成岩成矿作用. 中国地质调查, 10(4): 37-45. doi: 10.19388/j.zgdzdc.2023.04.05
引用本文: 袁和1, 白银增2, 耿树峰1, 洪秀伟1, 王登红3. 2023. 辽宁省重点金矿集区地质特征及成岩成矿作用. 中国地质调查, 10(4): 37-45. doi: 10.19388/j.zgdzdc.2023.04.05
YUAN He, BAI Yinzeng, GENG Shufeng, HONG Xiuwei, WANG Denghong. 2023. Geological characteristics, diagenesis and mineralization of key gold concentration areas in Liaoning Province. Geological Survey of China, 10(4): 37-45. doi: 10.19388/j.zgdzdc.2023.04.05
Citation: YUAN He, BAI Yinzeng, GENG Shufeng, HONG Xiuwei, WANG Denghong. 2023. Geological characteristics, diagenesis and mineralization of key gold concentration areas in Liaoning Province. Geological Survey of China, 10(4): 37-45. doi: 10.19388/j.zgdzdc.2023.04.05

辽宁省重点金矿集区地质特征及成岩成矿作用

  • 基金项目:

    中国地质调查局“中国矿产地质志(编号: DD20160346、DD20190379)”项目资助

详细信息
    作者简介: 袁和(1985—),男,高级工程师,主要从事矿床学研究工作。Email: yuanhe1985@126.com。
  • 中图分类号: P618.51;P612

Geological characteristics, diagenesis and mineralization of key gold concentration areas in Liaoning Province

  • 作为我国重要的产金省份,辽宁省的中生代构造、岩浆活动较为强烈,并伴有强烈的金成矿作用。根据金矿床的空间分布特征,将辽宁省划分出5个重点金矿集区,为深入了解各金矿集区内金矿床的成岩成矿作用,对金矿集区的地质特征、成岩成矿时代、地球化学等方面进行了系统分析。研究表明: 各金矿集区的金成矿作用与印支期、燕山期岩浆活动有关,成矿时间集中于126~118 Ma、225~188 Ma; 辽西金矿集区金矿石中的S属于地幔硫,而辽东金矿集区S来源于岩浆和变质岩地层,各矿集区矿石的Pb具有壳幔混合源特征,5个重点金矿集区的成矿物质源区组成为同一岩浆源区、不同岩浆演化阶段的产物,成岩成矿物质为下地壳部分熔融的产物,并有部分幔源物质参与。结合近年找矿进展,建立了辽宁省金矿找矿预测地质模型,可为下一步开展区域矿产勘查工作提供新思路。
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出版历程
收稿日期:  2022-06-27
修回日期:  2023-04-20

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