| 辽西沙锅屯-富隆山地区的加里东运动形迹 |
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| 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 |
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| 作者姓名： | 王志军 李红梅 王会中 |
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| 作者单位： | 辽宁省地质勘查院, 辽宁 大连 116100 |
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| 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.
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| 关 键 词： | 沙锅屯-富隆山地区 背斜 向斜 晚古生界 加里东运动 |
| 收稿时间： | 2010-04-13 |
| 修稿时间： | 2010-05-26 |
THE CALEDONIAN MOVEMENT OF SHAGUOTUN-FULONGSHAN AREA IN WESTERN LIAONING |
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| 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 |
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| Authors: | WANG Zhi-jun LI Hong-mei WANG Hui-zhong |
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| Affiliation: | Liaoning Institute of Geological Survey, Dalian 116100, Liaoning Province, China |
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| 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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| Keywords: | anticline syncline Late Paleozoic Caledonian movement Shaguotun-Fulongshan area Western Liaoning Province |
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