中国地质科学院地质力学研究所
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华南重要成矿区带中生代构造变形及其控岩控矿机理

张达, 李芳, 贺晓龙, 胡擘捷, 张鑫明, 毕珉烽, 王森, 霍海龙, 薛伟, 刘松岩. 2021. 华南重要成矿区带中生代构造变形及其控岩控矿机理. 地质力学学报, 27(4): 497-528. doi: 10.12090/j.issn.1006-6616.2021.27.04.045
引用本文: 张达, 李芳, 贺晓龙, 胡擘捷, 张鑫明, 毕珉烽, 王森, 霍海龙, 薛伟, 刘松岩. 2021. 华南重要成矿区带中生代构造变形及其控岩控矿机理. 地质力学学报, 27(4): 497-528. doi: 10.12090/j.issn.1006-6616.2021.27.04.045
ZHANG Da, LI Fang, HE Xiaolong, HU Bojie, ZHANG Xinming, BI Minfeng, WANG Sen, HUO Hailong, XUE Wei, LIU Songyan. 2021. Mesozoic tectonic deformation and its rock/ore-control mechanism in the important metallogenic belts in South China. Journal of Geomechanics, 27(4): 497-528. doi: 10.12090/j.issn.1006-6616.2021.27.04.045
Citation: ZHANG Da, LI Fang, HE Xiaolong, HU Bojie, ZHANG Xinming, BI Minfeng, WANG Sen, HUO Hailong, XUE Wei, LIU Songyan. 2021. Mesozoic tectonic deformation and its rock/ore-control mechanism in the important metallogenic belts in South China. Journal of Geomechanics, 27(4): 497-528. doi: 10.12090/j.issn.1006-6616.2021.27.04.045

华南重要成矿区带中生代构造变形及其控岩控矿机理

  • 基金项目:
    国家自然科学基金项目(41772069);国家重点研发计划项目(2016YFC0600509);中国地质调查局地质调查项目(12120113089600, 12120114028701, 1212011085472)
详细信息
    作者简介: 张达(1967-), 男, 教授, 博士生导师, 主要从事区域构造、构造地质及矿田构造教学研究工作。E-mail: zhangda@cugb.edu.cn
  • 中图分类号: P613

Mesozoic tectonic deformation and its rock/ore-control mechanism in the important metallogenic belts in South China

  • Fund Project: This research is financially supported by the National Natural Science Foundation of China (Grant No.41772069), the National Key Research and Development Program of China (Grant No.2016YFC0600509), and the Geological Survey Programs of China Geological Survey(Grant No.12120113089600, 12120114028701, 1212011085472)
  • 华南大陆中生代以来受华北板块、西南缘特提斯洋以及东部古太平洋板块会聚作用形成了多序次的构造变形及多期岩浆与成矿事件, 并造就了多个重要的多金属成矿区带。文章在梳理成矿区带典型矽卡岩型矿床矿化期次、矿体分布及成矿机理等关键科学问题的基础上, 利用构造变形序次及其控岩控矿的规律性完善了典型矿床成矿过程及成因机理。通过对闽西南铁多金属成矿带、赣东北塔前-赋春钨铜多金属成矿带以及滇东南老君山钨锡矿集区开展构造变形解析, 结合已有研究成果, 厘定出相对完整的印支期、中晚侏罗世及白垩纪3期变形序列, 但其作用时限、构造性质、规模强度及变形样式却表现不一。通过构造控岩分析并结合已有同位素年代学得出, 不同成矿区带都存在与变形序列相一致的岩浆或变质热事件, 进而利用变形序列与岩浆期次对应规律明确了与马坑式铁多金属矿床、朱溪钨铜矿床以及南秧田钨矿床相关的多期岩浆活动。在此基础上识别出多阶段矿化事件并提出3个典型矿床都存在多期叠加复合成矿的认识。从构造对矿床就位机制控制的角度分析了马坑式矿床分散多变矿体、朱溪矿床垂向大跨度矿化及深部巨型矿体、南秧田矿床层-脉叠加矿体分别受赋矿地层褶皱拆离、大规模双重逆冲以及2期构造变形复合控制的机理。文章最后探讨了不同阶段华南重要成矿区带构造变形及岩浆成矿的动力学背景。

  • 加载中
  • 图 1  华南主要构造格局与矿产分布图(据张岳桥等,2009毛景文等,2008修改)

    Figure 1. 

    图 2  闽西南地质构造与铁多金属矿床分布图(据张达等,2011修改)

    Figure 2. 

    图 3  闽西南马坑式铁多金属矿床矿体分布剖面示意图(据福建省地质调查院,2011修改)

    Figure 3. 

    图 4  塔前—赋春成矿带地质构造与矿产分布图(据陈国华等,2012修改)

    Figure 4. 

    图 5  朱溪钨铜矿床联合剖面图(据贺晓龙等,2018修改)

    Figure 5. 

    图 6  老君山矿集区及外围地质构造与矿产分布图(据毕珉烽等, 2015, 修改)

    Figure 6. 

    图 7  南秧田钨矿床0号勘探线剖面图(据有色地勘局317队资料,1984修改)

    Figure 7. 

    图 8  闽西南中生代构造变形特征

    Figure 8. 

    图 9  闽西南早中生代拆离变形及伴生褶皱特征

    Figure 9. 

    图 10  龙岩翠屏山一带拆离断层及其变形特征(据闽西地质大队,1989修改)

    Figure 10. 

    图 11  闽西南盆地西缘印支期推覆构造剖面图(据闽西地质大队,1989修改)

    Figure 11. 

    图 12  闽西南盆地西缘中侏罗世末推覆构造特征(D2-1)(据闽西地质大队,1989修改)

    Figure 12. 

    图 13  闽西南盆地中东部晚侏罗世推覆构造特征(D2-2)(据闽西地质大队,1989修改)

    Figure 13. 

    图 14  赣东北塔前-赋春钨铜多金属成矿带推覆构造变形特征

    Figure 14. 

    图 15  景德镇-鹄山推覆构造变形剖面图(剖面位置见图 4)

    Figure 15. 

    图 16  老君山矿集区构造变形特征

    Figure 16. 

    图 17  Song Chay穹窿多层次推覆变形及似层状矽卡岩矿体分布图

    Figure 17. 

    图 18  龙岩九峰崎推覆体与铁多金属矿床分布图

    Figure 18. 

    图 19  马坑外围推覆构造及其对矽卡岩型铁矿化体的控制

    Figure 19. 

    图 20  德化阳山受褶皱控制的矽卡岩矿体(据林全胜,2013修改)

    Figure 20. 

    图 21  塔前—赋春一带推覆构造控岩控矿特征

    Figure 21. 

    图 22  塔前—赋春一带推覆构造控岩控矿模式图

    Figure 22. 

    图 23  滇东南W-Sn成矿时代分布特征

    Figure 23. 

    图 24  老君山矿集区南秧田钨矿床2期构造控矿特征

    Figure 24. 

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出版历程
收稿日期:  2021-04-09
修回日期:  2021-06-05
刊出日期:  2021-08-25

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