| 华北板块西南缘义马盆地中侏罗世沉积相及古地理 |
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| 引用本文： | 高迪, 邵龙义, 王德伟, 李猛, 刘建国. 华北板块西南缘义马盆地中侏罗世沉积相及古地理[J]. 沉积与特提斯地质, 2016, 36(4): 7-13. |
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| 作者姓名： | 高迪 邵龙义 王德伟 李猛 刘建国 |
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| 作者单位： | 1.河南理工大学 资源环境学院,河南 焦作 454003; 2.中原经济区煤层 (页岩) 气河南协同创新中心,河南 焦作 454003; 3.中国矿业大学(北京)地球科学与测绘工程学院,北京 100083; 4.河南省煤炭地质勘察研究院,河南 郑州 450052 |
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| 基金项目： | 国家自然科学基金(41402094)、国家重大科技专项课题(2011ZX05009-002)、中国煤炭工业协会项目(MTKJ-2011-414)、河南理工大学博士基金(B2011-013)联合资助 |
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| 摘 要： | 义马盆地位于华北板块西南缘,是河南省境内唯一可采的中生代煤田,位置特殊。为了揭示其中侏罗世阿林期-巴柔期的沉积相及其古地理演化特征,运用矿物岩石学、地球化学、沉积学及岩相古地理等方法,以义马盆地中侏罗世含煤岩系为例,进行地层划分及沉积相和古地理研究。研究结果表明,研究区中侏罗世含煤岩系属阿林期-巴柔期,该时期主要发育冲积扇、辫状河、三角洲、湖泊等4种沉积相。利用单因素分析多因素综合作图法,以成煤期为节点,定量恢复了阿林期-巴柔期的古地理特征,从成煤期前到成煤期后,各优势古地理单元变化明显,具有冲积扇-三角洲-湖泊的变化规律,整体上是一个退积过程。
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| 关 键 词： | 沉积相 古地理 中侏罗世 华北板块西南缘 义马盆地 |
| 收稿时间： | 2016-05-30 |
| 修稿时间： | 2016-07-21 |
Middle Jurassic sedimentary facies and palaeogeography of the Yima Basin on the southwestern margin of the North China plate |
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| GAO Di, SHAO Long-yi, WANG De-wei, LI Meng, LIU Jian-guo. Middle Jurassic sedimentary facies and palaeogeography of the Yima Basin on the southwestern margin of the North China plate[J]. Sedimentary Geology and Tethyan Geology, 2016, 36(4): 7-13. |
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| Authors: | GAO Di SHAO Long-yi WANG De-wei LI Meng LIU Jian-guo |
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| Affiliation: | 1.Institute of Resources and Environments,Henan Polytechnic University,Jiaozuo 454003,Henan,China; 2.Collaborative Innovation Center of Coalbed Methane(Shale Gas) for Central Plains Economic Region,Jiaozuo 454003,Henan,China; 3.College of Geoscience and Surveying Engineering,China University of Mining&Technology,Beijing 100083,China; 4.Research Institute of Henan Coal Geological Exploration,Zhengzhou 450052,Henan,China |
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| Abstract: | The Yima basin located on the southwestern margin of the North China plate is the sole recoverable Mesozoic coal field in Henan. Exemplified by the Middle Jurassic coal measures, the stratigraphic division, sedimentary facies and palaeogeographic analysis are made on the basis of lithological, geochemical and sedimentological data. The Middle Jurassic coal measures belong to the Aalenian-Bajocian, when four sedimentary facies are developed, including the alluvial fan, braided stream, delta and lake facies. The Aalenian-Bajocian sedimentary facies and palaeogeographic maps are constructed with the aid of the single factor and multifactor mapping methods. The palaeogeographic units tend to display the variations of the alluvial fan, delta and lake facies, and represent a retrogradational process in the Yima basin throughout the coal-forming periods. |
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| Keywords: | sedimentary facies palaeogeography Middle Jurassic southwestern margin of the North China plate Yima basin |
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