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.
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.
WANG Zhi-jun, LI Hong-mei, WANG Hui-zhong. THE CALEDONIAN MOVEMENT OF SHAGUOTUN-FULONGSHAN AREA IN WESTERN LIAONING. GEOLOGY AND RESOURCES, 2010, 19(3): 221-223.
2010, Vol. 19 
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