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
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
THE CALEDONIAN MOVEMENT OF SHAGUOTUN-FULONGSHAN AREA IN WESTERN LIAONING
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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