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A Preliminary Report on Yong'anpu Tectonic Window in Suizhong County, Western Liaoning Province
引用本文:汪洋[,] 姬广义.A Preliminary Report on Yong'anpu Tectonic Window in Suizhong County, Western Liaoning Province[J].中国地质大学学报(英文版),2006,17(3):231-237.
作者姓名:汪洋[  ] 姬广义
作者单位:[1]Key Laboratory of Isotope Geochronology and Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China [2]School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China [3]Geological Institute of Beijing Municipality, Beijing 100011, China
基金项目:This paper is financially supported by the National Natural Science Foundation of China (Nos. 40572128, 40376013, 40104003).ACKN0WLEDGMENT This study was supported by the National Natural Science Foundation of China (Nos. 40572128, 40376013, 40104003).
摘    要:For understanding the Mesozoic tectonics of Yanshan (燕山 ) belt, the authors took geological mapping in the belt. A large-scale thrust structure was identified in Yonganpu (永安堡) area. in the western part of Suizhong (绥中 ) County, Liaoning (辽宁 ) Province during our recent mapping in the Yanshan belt. The hanging wall of the thrust was composed of Archean gneiss and the overlying Early Cretaceous Zhangjiakou (张家口 ) Formation; meanwhile, the strongly ductile deformed volcanic rocks of Zhangjiakou Formation comprised the footwall in Yong'anpu tectonic window. This discovery indicates the existence of strongly contractional deformation in the Yanshan belt after the eruption of Early Cretaceous Zhangjiakou volcanic rocks. On the basis of mapping and research, it is concluded that the published official geological maps have failed to identify the major structural features of the Yanshan belt.

关 键 词:冲断层结构  永安堡  辽宁  白垩纪
收稿时间:02 28 2006 12:00AM
修稿时间:06 25 2006 12:00AM

A Preliminary Report on Yonganpu Tectonic Window in Suizhong County,Western Liaoning Province
Wang Yang,Ji Guangyi.A Preliminary Report on Yonganpu Tectonic Window in Suizhong County,Western Liaoning Province[J].Journal of China University of Geosciences,2006,17(3):231-237.
Authors:Wang Yang  Ji Guangyi
Institution:Key Laboratory of Isotope Geochronology and Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China; School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China;Geological Institute of Beijing Municipality, Beijing 100011, China
Abstract:For understanding the Mesozoic tectonics of Yanshan (
></figure>) belt, the authors took geological mapping in the belt. A large-scale thrust structure was identified in Yonganpu (<figure class=></figure>) area, in the western part of Suizhong (<figure class=></figure>) County, Liaoning (<figure class=></figure>) Province during our recent mapping in the Yanshan belt. The hanging wall of the thrust was composed of Archean gneiss and the overlying Early Cretaceous Zhangjiakou (<figure class=></figure>) Formation; meanwhile, the strongly ductile deformed volcanic rocks of Zhangjiakou Formation comprised the footwall in Yonganpu tectonic window. This discovery indicates the existence of strongly contractional deformation in the Yanshan belt after the eruption of Early Cretaceous Zhangjiakou volcanic rocks. On the basis of mapping and research, it is concluded that the published official geological maps have failed to identify the major structural features of the Yanshan belt.</td>
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Keywords:thrust structure  refolding  structural mapping  Early Cretaceous  Yonganpu  
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