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    南岭构造带基础地质特征与成矿地质背景

    徐先兵 梁承华 陈家驹 徐亚东

    徐先兵, 梁承华, 陈家驹, 徐亚东, 2021. 南岭构造带基础地质特征与成矿地质背景. 地球科学, 46(4): 1133-1150. doi: 10.3799/dqkx.2020.151
    引用本文: 徐先兵, 梁承华, 陈家驹, 徐亚东, 2021. 南岭构造带基础地质特征与成矿地质背景. 地球科学, 46(4): 1133-1150. doi: 10.3799/dqkx.2020.151
    Xu Xianbing, Liang Chenghua, Chen Jiaju, Xu Yadong, 2021. Fundamental Geological Features and Metallogenic Geological Backgrounds of Nanling Tectonic Belt. Earth Science, 46(4): 1133-1150. doi: 10.3799/dqkx.2020.151
    Citation: Xu Xianbing, Liang Chenghua, Chen Jiaju, Xu Yadong, 2021. Fundamental Geological Features and Metallogenic Geological Backgrounds of Nanling Tectonic Belt. Earth Science, 46(4): 1133-1150. doi: 10.3799/dqkx.2020.151

    南岭构造带基础地质特征与成矿地质背景

    doi: 10.3799/dqkx.2020.151
    基金项目: 

    中国地质调查局项目 DD20190811

    详细信息
      作者简介:

      徐先兵(1983-), 男, 副教授, 博士, 主要从事构造地质学的教学与科研工作.ORCID: 0000-0002-5341-9492.E-mail: xbxu2011@cug.edu.cn

    • 中图分类号: P56

    Fundamental Geological Features and Metallogenic Geological Backgrounds of Nanling Tectonic Belt

    • 摘要: 南岭构造带横跨扬子地块、江南造山带以及华夏地块,是中国钨锡铅锌铀等有色金属和铌钽锂铯与稀土等关键金属成矿带.通过综述近十五年来的研究进展,总结了南岭构造带基础地质特征与成矿地质背景.扬子与华夏地块沿永州-桂林-柳州一线于新元古代拼合,但缺乏直接的地质证据,需对龙胜蛇绿混杂岩和鹰扬关混杂岩进行深入研究.新元古代至中生代花岗岩二阶段模式年龄TDM2值揭示2.0~1.2 Ga为南岭构造带的主要地壳增生期.相似的花岗岩特征和构造线方向指示广西期和印支期造山机制均为陆内造山作用,是华南大陆南侧不同板块之间拼贴远程应力场的产物.燕山早期花岗岩εHf(t)值沿南岭构造带自西向东显著减小,而TDM2值明显增加,指示湘南-桂北-粤北地区在晚侏罗世经历了古太平洋板块断离和软流圈上涌并发育强烈的壳幔相互作用,为南岭构造带东段华夏地块上钨锡等多金属成矿提供了成矿物质来源和有利的伸展构造背景.南岭构造带西段扬子地块构造相对稳定且显生宙岩浆活动较弱,新元古代大塘坡组和寒武系底部页岩是良好的页岩气勘探目标.综合沉积、岩浆以及构造变形,华南中生代特提斯构造域向古太平洋构造域转换开始于晚三叠世.

       

    • 图  1  南岭构造带地形-地貌数字高程模型

      Fig.  1.  Digital elevation map of the Nanling tectonic belt, South China

      图  2  南岭构造带大地构造位置示意图与地质简图

      F1.萍乡-江山-绍兴断裂; F2.茶陵-郴州-临武-鹰扬关-梧州断裂; F3.永州-桂林-柳州断裂; F4.安化-罗城断裂; F5.怀化-凯里断裂; F6.鹰潭-安远-韶关-清远断裂; F7.会昌-河源断裂; F8.梧州-四会隐伏断裂; F9.茶陵-广昌断裂

      Fig.  2.  Location of tectonic map and sketch geological map of the Nanling tectonic belt

      图  3  南岭构造带新元古代至早古生代地层柱状图

      Fig.  3.  Neoproterozoic to Early Paleozoic stratigraphic column of Nanling tectonic belt

      图  4  南岭构造带中酸性侵入岩锆石U-Pb年龄分布(a)与年龄-经度分布(b)

      Fig.  4.  Detrital zircon age patterns for granitoids (a) and diagram of age vs. longitude (b) for the Nanling tectonic belt, South China

      图  5  南岭构造带花岗岩εHf(t)、TDM2 vs. 年龄和经度分布

      Fig.  5.  Diagrams of εHf(t) vs. longitude (a), εHf(t) vs. age (b), TDM2 vs. longitude (c) and TDM2 vs. age (d) for the Nanling tectonic belt, South China

      图  6  南岭构造带构造纲要

      Fig.  6.  Tectonic outline map of the Nanling tectonic belt, South China

      图  7  南岭构造带钨锡铌钽铀矿与稀土矿分布

      Fig.  7.  W-Sn-Nb-Ta-U and REE deposites in the Nanling tectonic belt

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