| 陕北地区中侏罗世延安期古地理特征* |
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| 引用本文： | 王东东,邵龙义,李智学,李兆彬.陕北地区中侏罗世延安期古地理特征*[J].古地理学报,2012,14(4):451-460. |
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| 作者姓名： | 王东东 邵龙义 李智学 李兆彬 |
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| 作者单位： | 1.中国矿业大学（北京）地球科学与测绘工程学院，北京 100083;2.陕西省煤田地质局勘察研究院，陕西西安 710054 |
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| 基金项目： | 河南省生物遗迹与成矿过程重点实验室开放基金项目，国家科技重大专项 |
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| 摘 要： | 在系统收集陕北地区中侏罗统延安组野外露头、钻井、测井、古生物等资料的基础上，对延安组沉积期的沉积环境及其层序地层格架进行分析，并恢复了各层序沉积期的岩相古地理格局。将延安组划分为3个三级层序，分层序绘制了关键单因素的等值线图，恢复了各层序沉积期的岩相古地理格局。层序Ⅰ沉积早期主要为河流沉积；随着盆地沉降的加剧，中部地区逐渐变为湖泊沉积，东北部河流沉积演变为三角洲沉积；层序Ⅱ沉积时期基本继承了层序Ⅰ晚期的沉积格局，古地理格局相对较稳定；层序Ⅲ沉积期，盆地基底不断抬升，湖泊逐渐萎缩成局限湖，河流沉积、三角洲沉积分别在研究区中部、东北部大规模发育。
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| 关 键 词： | 沉积相 层序地层 古地理 延安期 陕北地区 |
| 收稿时间： | 2011-03-29 |
Palaeogeographic characteristics of the Middle Jurassic Yan'an Age in northern Shaanxi Province |
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| Wang Dongdong
,
Shao Longyi
,
Li Zhixue
,
Li Zhaobin.Palaeogeographic characteristics of the Middle Jurassic Yan'an Age in northern Shaanxi Province[J].Journal of Palaeogeography,2012,14(4):451-460. |
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| Authors: | Wang Dongdong Shao Longyi Li Zhixue Li Zhaobin |
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| Institution: | 1.College of Geoscience and Surveying Engineering，China University of Mining and Technology(Beijing)，Beijing 100083;2.Investigation Academy of Shaanxi Coalfield Geology Bureau，Xi′an 710054，Shaanxi |
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| Abstract: | This paper systematically collected some basic data including outcrops， wells，loggings，paleontological data， etc. Based on those data，the sedimentary environments and sequence stratigraphic framework of the Middle Jurassic Yan′an Formation were analyzed，and the lithofacies palaeogeography map of each sequence was drawn.In this paper，the Yan′an Formation can be divided into 3 third-order sequences and taken as the drawing unit.Based on this，some key single factors isoline maps were drawn.By analyzing all the single factors synthetically，the lithofacies palaeogeographic maps of each sequence were reconstructed.During the early depositional period of the sequence Ⅰ，the fluvial deposits were developed.Then，the basin sedimentation aggravated，the deposits of the basin center gradually changed into lacustrine deposits. The sedimentary framework of the sequence II basically inherited that of the late period of sequence Ⅰ，and the palaeogeographic patterns were relatively stable.During the depositional period of sequence Ⅲ，the basin basement continuously lifted，the lake gradually changed into limited lake，and the fluvial and the delta deposits were mainly developed in the middle and northeastern area of the study area respectively. |
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| Keywords: | sedimentary facies sequence stratigraphy palaeogeography Yan′an Age northern Shaanxi Province |
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