济阳坳陷中生界中下侏罗统沉积相特征

英文篇名：The Sedimentary Facies and Paleogeographical Distributions of the Mesozoic in Jiyang Depression
中文刊名：中国科技信息
英文刊名：China Science and Technology Information
作者：宫诲婕 ; 李增学 ; 张晖
英文作者：Gong Huijie1 Li Zengxue2 Zhang Hui3 1 ; School of Earth Sciences and Resources ; China University of Geosciences ; Beijing 100083 ; China ; 2 ; College of Geo-Information Science and Engineering ; Shandong University of Science and Technology ; Qingdao ; Shandong 266510 ; China ; 3 ; Shandong Provincial of Coal Geology ; Taian ; Shandong 271000
中文关键词：中生代 ; 沉积相 ; 沉积体系 ; 济阳坳陷
英文关键词：Mesozoic ; Sedimentary facies ; Depositional system ; Jiyang Depression
出版日期：2010-01-01
机构：中国地质大学(北京)地球科学与资源学院;山东科技大学地质科学与工程学院;山东省煤田地质局第三勘探队;
年：2010
期：01
出版单位：中国科技信息

摘要

通过钻井、测井、地震等资料的分析,采用沉积学、地层学、古生物学、地球化学、岩石学等多学科综合的方法,对济阳探区中生界沉积特征、相及沉积体系进行了较为全面、系统的研究。研究表明,济阳坳陷中生代主要发育六种沉积相类型及相组合,即冲积扇相组合、河流相组合、三角洲体系及相组合、滨浅湖相、湖湾相、沼泽相。济阳坳陷中生代坊子组时期以滨浅湖沉积为主;三台组主要发育冲积平原亚相。
Based on the analyzing the data of the well,logging,seismic,sedimentary characteristics,facies and depositional system of the exploration area in Mesozoic of Jiyang Depression.are studied in detailed by the way of sedimentology,stratigraphy,paleontology,geochemistry,petrology and multidisciplinary integrated method. The results show that Jiyang Depression mainly developed six types of sedimentary facies and facies group,namely alluvial fan facies group,fluvial facies group,delta system and facies group,shallow lake facies,arm of lake facies and swamp. During the period of Fangzi Formation,there is mainly shallow-lake sediment; During the period of Santai Formation,it mainly developed alluvial plain subfacies; During the period of Mengyin Formation it principal developed littoral and shallow lake subfacies and alluvial plain subfacies. And fan delta facies was more than the one of the period of Santai Formation.

引文

[1]侯贵廷,钱祥麟,蔡东升.渤海湾盆地中、新生代构造演化研究[J].北京大学学报(自然科学版).2001,37(6):428～434
    [2]李丕龙.胜利油区勘探现状及展望[J].油气地质与采收率,2002,9(1):912.
    [3]苏宗富,邓宏文,陶宗普等.济阳坳陷古近系区域层序地层格架地层特征对比[J].古地理学报.2006,8(1):89-102
    [4]王世虎,夏斌,陈根文等.济阳坳陷构造特征及形成机制讨论[J].大地构造与成矿学.2004,28(4):428～434
    [5]王颖,赵锡奎,高博禹,等.济阳坳陷构造演化特征[J].成都理工学院学报,2002,29(2):181-187.
    [6]吴智平,侯旭波,李伟.华北东部地区中生代盆地格局及演化过程探讨[J].大地构造与成矿学.2007,31(4):385～389
    [7]吴智平,李伟,任拥军,等.济阳坳陷中生代盆地演化及其与新生代盆地叠合关系探讨[J].地质学报.2003,77(2):280-286.
    [8]徐振中,陈世悦,姜佩仁.济阳坳陷早中侏罗世沉积特征与沉积模式[J].吉林大学学报(地球科学版).2005,35(6):738～744
    [9]徐振中,陈世悦,姚军等.济阳坳陷中生代物源方向与沉积体系[J].沉积与特提斯地质.2008,28(2):83-88
    [10]杨超,陈清华.济阳坳陷构造演化及其构造层的划分[J].油气地质与采收率.2005,12(2):9-12,22.
    [11]宗国洪,施央申.济阳坳陷构造演化及其大地构造意义[J].高校地质学报.1999,5(3):275-282.