| 华北陆块东南缘凤台组时代的讨论 |
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| 引用本文： | 曹高社,张善文,柳忠泉,杨晓勇,刘德良.华北陆块东南缘凤台组时代的讨论[J].地质科学,2006,41(4):720-728. |
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| 作者姓名： | 曹高社 张善文 柳忠泉 杨晓勇 刘德良 |
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| 作者单位： | 1. 河南理工大学资源与环境学院, 河南, 焦作, 454000;2. 胜利石油管理局地质科学研究院, 山东, 东营, 257001;3. 中国科学技术大学地球与空间科学学院, 合肥, 230026 |
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| 基金项目： | 国家自然科学基金，国家重点基础研究发展计划(973计划) |
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| 摘 要： | 华北陆块东南缘凤台组归属于震旦系或寒武系尚无定论,影响了对华北陆块震旦纪与寒武纪转折时期的古构造、古地理和古生物的重大质变事件的探讨。本文根据下震旦统顶部与凤台组之间裂离不整合的发现及其意义的讨论,以及凤台组夹层粉砂质泥岩620Ma的Pb-Pb等时线年龄,基本厘定出凤台组时代为晚震旦世。
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| 关 键 词： | 凤台组 裂离不整合 Pb-Pb等时线 晚震旦世 华北陆块 |
| 文章编号： | 0563-5020（2006）04-0720-09 |
| 收稿时间： | 2005-04-11 |
| 修稿时间： | 2005-11-04 |
DISCUSSION ON AGE OF THE FENGTAI FORMATION ALONG SOUTHEASTERN MARGIN OF THE NORTH CHINA BLOCK |
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| Cao Gaoshe,Zhang Shanwen,Liu Zhongquan,Yang Xiaoyong,Liu Deliang.DISCUSSION ON AGE OF THE FENGTAI FORMATION ALONG SOUTHEASTERN MARGIN OF THE NORTH CHINA BLOCK[J].Chinese Journal of Geology,2006,41(4):720-728. |
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| Authors: | Cao Gaoshe Zhang Shanwen Liu Zhongquan Yang Xiaoyong Liu Deliang |
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| Institution: | 1. School of Resources and Environment, Henan Polytechnic University, Jiaozuo, Henan 454000;2. Geological Scientific Research Institute of Shengli Oilfield, Dongying, Shandong 257015;3. School of Earth and Space Sciences, China University of Science and Technology, Hefei 230026 |
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| Abstract: | There was an argument about age of the Fengtai Formation being Sinian or Cambrian. Based on the discovery of breakup uncomformity between the Lower Sinian Sidingshan Formation and the Fengtai Formation, the field features and geochemical evidence of the unconformity, and the Pb-Pb isochronal dating of silt mudstone interbeds from the Fengtai Formation being 620 Ma, the paper thought that the Fengtai Formation should be deposits of Late Sinian. This result might stimulate the study of paleostructure, paleogeography and paleontology in the transitional period between the Sinian and Cambrian in the North China Block. |
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| Keywords: | The Fengtai Formation Breakup uncomformity Pb-Pb isochron Late Sinian The North China Block |
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