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福建紫金山矿田早白垩世以来构造演化和成岩成矿时空格架

潘天望 袁远 吕勇 史文强

潘天望, 袁远, 吕勇, 等, 2019. 福建紫金山矿田早白垩世以来构造演化和成岩成矿时空格架. 地质力学学报, 25 (1): 61-76. DOI: 10.12090/j.issn.1006-6616.2019.25.01.007
引用本文: 潘天望, 袁远, 吕勇, 等, 2019. 福建紫金山矿田早白垩世以来构造演化和成岩成矿时空格架. 地质力学学报, 25 (1): 61-76. DOI: 10.12090/j.issn.1006-6616.2019.25.01.007
PAN Tianwang, YUAN Yuan, LYU Yong, et al., 2019. THE EARLY-CRETACEOUS TECTONIC EVOLUTION AND THE SPATIAL-TEMPORAL FRAMEWORK OF MAGMATISM-MINERALIZATION IN ZIJINSHAN ORE-FIELD, FUJIAN PROVINCE. Journal of Geomechanics, 25 (1): 61-76. DOI: 10.12090/j.issn.1006-6616.2019.25.01.007
Citation: PAN Tianwang, YUAN Yuan, LYU Yong, et al., 2019. THE EARLY-CRETACEOUS TECTONIC EVOLUTION AND THE SPATIAL-TEMPORAL FRAMEWORK OF MAGMATISM-MINERALIZATION IN ZIJINSHAN ORE-FIELD, FUJIAN PROVINCE. Journal of Geomechanics, 25 (1): 61-76. DOI: 10.12090/j.issn.1006-6616.2019.25.01.007

福建紫金山矿田早白垩世以来构造演化和成岩成矿时空格架

doi: 10.12090/j.issn.1006-6616.2019.25.01.007
基金项目: 

中国地质调查局地质调查项目 DD20160061

中国地质调查局地质调查项目 DD20179313

详细信息
    作者简介:

    潘天望(1988-), 男, 研究实习员, 主要从事构造地质学与岩溶洞穴景观研究。E-mail:pantianwang@kasrt.ac.cn

    通讯作者:

    袁远(1989-), 男, 在读博士, 矿田构造专业。E-mail:y_yuan0731@163.com

  • 中图分类号: P548;P612

THE EARLY-CRETACEOUS TECTONIC EVOLUTION AND THE SPATIAL-TEMPORAL FRAMEWORK OF MAGMATISM-MINERALIZATION IN ZIJINSHAN ORE-FIELD, FUJIAN PROVINCE

  • 摘要: 在充分吸收已有工作成果的基础上,文章系统总结了紫金山矿田的典型矿床类型及特征,探讨了早白垩世伸展构造背景下该矿田成岩成矿作用与北西向上杭—云霄成矿带的关系,并建立了早白垩世(145 Ma~)到晚白垩世早期(~92 Ma)紫金山矿田成岩成矿作用的时空格架。研究认为由于古太平洋板块俯冲作用体系的影响,早白垩世以来(145 Ma~)紫金山矿田总体上受北西向上杭—云霄深断裂多次活化作用的控制,依次经历了145~120 Ma伸展初期小规模的岩浆—成矿活动、125~110 Ma短暂的岩浆间歇期、110~92 Ma幔源物质大规模参与的岩浆活动及相应的斑岩型—浅成低温热液型(Cu-Au-Mo-Ag)多金属成矿作用。

     

  • 图  1  福建上杭—云霄成矿带区域地质与中生代火山盆地分布示意图

    a—区域地质简图[13];b—中生代火山盆地分布示意图[14, 21]

    Figure  1.  Tectonic location and regional geological map of Mesozoic Volcanic Basin in the regions of the Shanghang-Yunxiao mineralization belt, Fujian Province

    图  2  紫金山矿田区域地质简图与地质矿产略图

    a—区域地质简图[15];b—矿田地质矿产略图[2]

    Figure  2.  Regional geological map and mineral map of the Zijinshan ore-field

    图  3  早白垩世晚期—晚白垩世早期(110~92 Ma)紫金山Cu-Au-Mo-Ag矿田成矿模式图与地球动力学模型简图

    a—成矿模式图[3]; b—地球动力学模型简图[6, 34, 67]

    Figure  3.  Metallogenic pattern and Cartoon showing the possible tectonic setting for the porphyry-epithermal Cu-Au-Mo-Ag mineralization in the Zijinshan ore-field during 110~92 Ma

    表  1  上杭紫金山矿田中生代岩浆岩同位素年代一览表

    Table  1.   Mesozoic magmatic isotope dating of the Zijinshan ore-field

    时代 岩体名称 定年方法 测定对象 年龄/Ma 参考文献 相关矿床 定年方法 成因类型 年龄/Ma 参考文献
    早—晚白垩世 大岩里花岗斑岩脉 SHRIMP 锆石 93±2 [5]
    紫金山铜金矿床石英斑岩脉 SHRIMP 锆石 96±2 [5]
    浸铜湖石英正长斑岩脉 LA-ICP-MS U-Pb 锆石 95.3±2.1~96.7±0.9 [28] 浸铜湖Cu-Mo矿 斑岩型 [28]
    南山坪正长岩脉 LA-ICP-MS U-Pb 锆石 92.7±1.0 [9]
    南山坪正长斑岩脉 LA-ICP-MS U-Pb 锆石 97.3±1.2 [9]
    南山坪石英正长斑岩脉 LA-ICP-MS U-Pb 锆石 99.5±1.2 [9]
    晚期罗卜岭花岗闪长斑岩 LA-ICP-MS U-Pb 锆石 96.7±2.1 [29]
    罗卜岭深部花岗闪长岩基 SHRIMP 锆石 100±2 [5] 罗卜岭Cu-Mo矿 辉钼矿Re-Os 斑岩型 103~105 [6, 25]
    石帽山群下段气孔状英安岩 SHRIMP 锆石 102±1 [5]
    石帽山群上段上部流纹岩 LA-ICP-MS U-Pb 锆石 102±1 [6]
    紫金山深部花岗闪长岩 SHRIMP 锆石 102±2 [5]
    早期罗卜岭花岗闪长斑岩 LA-ICP-MS U-Pb 锆石 102.9±0.9 [29]
    紫金山深部花岗闪长斑岩 SHRIMP 锆石 103±2 [5]
    早期紫金山铜金矿床英安玢岩 LA-ICP-MS U-Pb 锆石 104±1~104±0.1 [6]
    早期紫金山铜金矿床英安玢岩 LA-ICP-MS U-Pb 锆石 105±0.7 [30]
    石帽山群上段上部流纹质晶屑凝灰岩 LA-ICP-MS U-Pb 锆石 105±0.1 [6]
    石帽山群下段安山岩 SHRIMP 锆石 106±2 [5]
    四方花岗闪长岩 LA-ICP-MS U-Pb 锆石 104.8±1.7 [31]
    Ar-Ar坪年龄 角闪石 104.8±0.8 [11]
    LA-ICP-MS U-Pb 锆石 107±1.8 [11]
    SHRIMP 锆石 109±2 [5]
    LA-ICP-MS U-Pb 锆石 112±1 [6]
    石帽山群下段中部凝灰熔岩 LA-ICP-MS U-Pb 锆石 108±1 [6]
    石帽山群下段上部凝灰岩 LA-ICP-MS U-Pb 锆石 110±1 [6]
    石帽山群上组下段流纹岩 LA-ICP-MS U-Pb 锆石 110.0±1.9 [4]
    紫金山铜金矿床英安玢岩 LA-ICP-MS U-Pb 锆石 110±0.4 [6]
    紫金山次火山岩 锆石U-Pb 锆石 118±4 [32] 有待考证
    石帽山群下组下段英安岩 LA-ICP-MS U-Pb 锆石 111±0.3~110±1 [6]
    石帽山群下段底部熔结角砾(集块)岩 LA-ICP-MS U-Pb 锆石 113.0±1.9 [4]
    中—晚侏罗世 才溪中粗粒似斑状二长花岗岩 LA-ICP-MS U-Pb 锆石 146.4±8.6 [31]
    SHRIMP 锆石 150±2 [5]
    SHRIMP 锆石 150±3 [30]
    金龙桥细粒花岗岩 LA-ICP-MS U-Pb 锆石 157±1 [6]
    LA-ICP-MS U-Pb 锆石 155 [33]
    SHRIMP 锆石 149±2 [5]
    LA-ICP-MS U-Pb 锆石 146.3±1.6 [4]
    五龙寺中细粒花岗岩 LA-ICP-MS U-Pb 锆石 164±1 [6]
    LA-ICP-MS U-Pb 锆石 163 [33]
    LA-ICP-MS U-Pb 锆石 149.3±1.6 [4]
    SHRIMP 锆石 149±2 [5]
    迳美中粗粒花岗岩 LA-ICP-MS U-Pb 锆石 165±1 [6]
    LA-ICP-MS U-Pb 锆石 164 [33]
    LA-ICP-MS U-Pb 锆石 157.9±1.2 [4]
    SHRIMP 锆石 154±2 [5]
    溪南二长花岗岩 LA-ICP-MS U-Pb 锆石 156.9±1.0 [34] 溪南Cu-Mo矿 辉钼矿Re-Os 斑岩型 108 [34]
    下载: 导出CSV

    表  2  紫金山矿田燕山期构造演化一览表

    Table  2.   Yanshanian tectonic evolution of the Zijinshan ore-field

    构造演化阶段 地质时代 代表性岩体(脉) 岩石成因 构造背景
    燕山晚期 早白垩世早期(145~120 Ma) 外围大洋-莒舟岩体 壳源岩石重熔,少量幔源组分参与 伸展构造背景(转换过渡)
    早白垩世中期(120~110 Ma) 岩浆间歇期 —— 短暂的构造反转
    早白垩世晚期(110~92 Ma) 四方岩体;罗卜岭岩体;大岩里花岗斑岩脉;紫金山石英斑岩脉;浸铜湖石英正长斑岩脉 地幔组分逐渐增多,具典型的壳幔混源型花岗岩特征 伸展环境,伸展作用逐渐加强,期间可能经历了短暂构造反转,
    下载: 导出CSV
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  • 收稿日期:  2017-10-10
  • 修回日期:  2018-05-22
  • 刊出日期:  2019-02-01

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