胡健民, 赵越, 刘晓文, 石玉若, 赵国春. 2005: 辽西凌源地区水泉沟组辉石安山岩锆石SHRIMP U-Pb定年及其意义. 地质通报, 24(2): 104-109.
    引用本文: 胡健民, 赵越, 刘晓文, 石玉若, 赵国春. 2005: 辽西凌源地区水泉沟组辉石安山岩锆石SHRIMP U-Pb定年及其意义. 地质通报, 24(2): 104-109.
    HU Jianmin, ZHAO Yue, LIU Xiaowen, SHI Yuruo, ZHAO Guochun. 2005: SHRIMP U-Pb dating for zircons from pyroxene andesite of Shuiquangou Formation in western Liaoning province and its tectonic significance. Geological Bulletin of China, 24(2): 104-109.
    Citation: HU Jianmin, ZHAO Yue, LIU Xiaowen, SHI Yuruo, ZHAO Guochun. 2005: SHRIMP U-Pb dating for zircons from pyroxene andesite of Shuiquangou Formation in western Liaoning province and its tectonic significance. Geological Bulletin of China, 24(2): 104-109.

    辽西凌源地区水泉沟组辉石安山岩锆石SHRIMP U-Pb定年及其意义

    SHRIMP U-Pb dating for zircons from pyroxene andesite of Shuiquangou Formation in western Liaoning province and its tectonic significance

    • 摘要: 水泉沟组分布在辽西凌源地区,不整合覆盖早中生代第一期推覆构造系统,其上又被稍晚形成的燕山早期推覆构造所掩覆.水泉沟组辉石安山岩锆石SHRIMP U-Pb测年结果为230.4Ma±3.1Ma.测试结果表明①辽西水泉沟组时代为晚三叠世;②燕山地区晚三叠世安山质火山岩很可能代表一种拉张的构造环境;③燕山地区早中生代早期挤压逆冲构造发育于早中三叠世,即燕山地区印支阶段早期为挤压逆冲,晚期为伸展构造.

       

    /

    返回文章
    返回