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    王志军, 李红梅, 王会中. 辽西沙锅屯-富隆山地区的加里东运动形迹[J]. 地质与资源, 2010, 19(3): 221-223. DOI: 10.13686/j.cnki.dzyzy.2010.03.002
    引用本文: 王志军, 李红梅, 王会中. 辽西沙锅屯-富隆山地区的加里东运动形迹[J]. 地质与资源, 2010, 19(3): 221-223. DOI: 10.13686/j.cnki.dzyzy.2010.03.002
    shu
    WANG Zhi-jun, LI Hong-mei, WANG Hui-zhong. THE CALEDONIAN MOVEMENT OF SHAGUOTUN-FULONGSHAN AREA IN WESTERN LIAONING[J]. Geology and Resources, 2010, 19(3): 221-223. DOI: 10.13686/j.cnki.dzyzy.2010.03.002
    Citation: WANG Zhi-jun, LI Hong-mei, WANG Hui-zhong. THE CALEDONIAN MOVEMENT OF SHAGUOTUN-FULONGSHAN AREA IN WESTERN LIAONING[J]. Geology and Resources, 2010, 19(3): 221-223. DOI: 10.13686/j.cnki.dzyzy.2010.03.002
    shu

    辽西沙锅屯-富隆山地区的加里东运动形迹

    THE CALEDONIAN MOVEMENT OF SHAGUOTUN-FULONGSHAN AREA IN WESTERN LIAONING

      摘要
    • 摘要: 沙锅屯-富隆山地区的下古生界组成东西向两个完整的背斜和一个向斜，其上被晚古生界以大角度不整合覆盖.该地区既有抬升造陆运动，又有挤压造山运动，运动时代加里东期.主要依据是本区的褶皱被石炭纪本溪组以大角度不整合覆盖，且有化石资料证明在华北板块内本溪组下部有下石炭世甚至泥盆纪地层.

       

      Abstract: The Lower Paleozoic strata in the Shaguotun-Fulongshan area form two complete anticlines and one syncline, which trend east-west, covered by Carboniferous Benxi formation with large angular unconformity. This area has experienced both uplifting continent-making movement and compressive orogenic movement, which took place during Caledonian epoch. The conclusion is supported by fossil data.

       

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