关于秦岭造山带

张国伟, 郭安林, 董云鹏, 姚安平. 关于秦岭造山带[J]. 地质力学学报, 2019, 25(5): 746-768. doi: 10.12090/j.issn.1006-6616.2019.25.05.064
引用本文: 张国伟, 郭安林, 董云鹏, 姚安平. 关于秦岭造山带[J]. 地质力学学报, 2019, 25(5): 746-768. doi: 10.12090/j.issn.1006-6616.2019.25.05.064
ZHANG Guowei, GUO Anlin, DONG Yunpeng, YAO Anping. RETHINKING OF THE QINLING OROGEN[J]. Journal of Geomechanics, 2019, 25(5): 746-768. doi: 10.12090/j.issn.1006-6616.2019.25.05.064
Citation: ZHANG Guowei, GUO Anlin, DONG Yunpeng, YAO Anping. RETHINKING OF THE QINLING OROGEN[J]. Journal of Geomechanics, 2019, 25(5): 746-768. doi: 10.12090/j.issn.1006-6616.2019.25.05.064

关于秦岭造山带

  • 基金项目:
    国家自然科学基金(49732080);西北大学院士工作室项目(134890003)
详细信息
    作者简介: 张国伟(1939-), 男, 教授, 中国科学院院士, 从事大陆造山带和前寒武纪地质研究。E-mail:gwzhang@nwu.edu.cn
  • 中图分类号: P54

  • 责任编辑:吴芳

RETHINKING OF THE QINLING OROGEN

  • 纪念老一代地球科学家李四光先生,思考地球科学与大地构造学的创新发展。文章以秦岭造山带为例思考大陆复合造山及其动力学,认知概括秦岭造山带基本属性与特质,探索认识中小多板块多期洋陆俯冲造山-陆-陆板块俯冲碰撞造山的板块复合造山,并又强烈叠加复合陆内造山,造成复杂组成与结构,形成立交桥式四维流变学分层的多层非耦合动态演化的大陆复合造山带模型,及其新的演化趋势动态和构成国家人类需求的成矿成藏物质财富与宜居的地表系统环境等,期望前瞻探索认知地球发展的未来。文章还就秦岭造山带几个有争议的问题,进行简要讨论,共求新的探索研究发展。期盼学习李四光先生学术理论精华,尤其在深化发展板块构造,探索认知大陆构造与动力学方面,创新发展地质力学,以宇宙太阳系视野探索地球动力学,推动大地构造新发展。

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  • 图 1  秦岭造山带构造单元划分图

    Figure 1. 

    图 2  秦岭造山带演化示意图

    Figure 2. 

    图 3  秦岭造山带岩石圈现今“立交桥”式结构模型

    Figure 3. 

    图 4  中国大地构造最新演化动态格局

    Figure 4. 

    图 5  秦岭-大别等中央造山系东西岩石圈剥露剖面示意图

    Figure 5. 

    图 6  秦岭-大别南缘勉略断裂构造带与勉略板块缝合带简图

    Figure 6. 

    图 7  秦岭及邻区二叠纪长兴期古地理

    Figure 7. 

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出版历程
收稿日期:  2019-09-28
修回日期:  2019-10-02
刊出日期:  2019-10-31

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