高级搜索

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

湖泊水下扇沉积特征及影响因素——以伊通盆地莫里青断陷双阳组为例

刘招君

downloadPDF
文章导航 > 沉积学报  > 2003 >  21(1): 148-154
刘招君. 湖泊水下扇沉积特征及影响因素——以伊通盆地莫里青断陷双阳组为例[J]. 沉积学报, 2003, 21(1): 148-154.
引用本文: 刘招君. 湖泊水下扇沉积特征及影响因素——以伊通盆地莫里青断陷双阳组为例[J]. 沉积学报, 2003, 21(1): 148-154.
shu
LIU Zhao-jun. Lacus Subaqueous Fan Sedimentary Characteristics and Influence Factors——A Case Study of Shuangyang Formation in Moliqing Fault Subsidence of Yitong Basin[J]. Acta Sedimentologica Sinica, 2003, 21(1): 148-154.
Citation: LIU Zhao-jun. Lacus Subaqueous Fan Sedimentary Characteristics and Influence Factors——A Case Study of Shuangyang Formation in Moliqing Fault Subsidence of Yitong Basin[J]. Acta Sedimentologica Sinica, 2003, 21(1): 148-154.
shu

湖泊水下扇沉积特征及影响因素——以伊通盆地莫里青断陷双阳组为例

  • 吉林大学地球科学学院 长春130061

详细信息

  • 中图分类号: P512.2

Lacus Subaqueous Fan Sedimentary Characteristics and Influence Factors——A Case Study of Shuangyang Formation in Moliqing Fault Subsidence of Yitong Basin

  • College of Earth Science, Jilin University, Changchun 130061

    摘要
  • 摘要: 伊通盆地莫里青断陷始新统双阳组发育典型的湖泊水下扇体。根据岩心、测井和地震资料 ,并结合粒度分析等方法 ,将其划分为内扇、中扇和外扇亚相及某干微相。影响水下扇形成和分布的主要因素是 :同生断裂的活动造就了陡坡地形 ,其幕式活动成为水下扇形成的触发机制 ;阵发型水下扇主要发育在陡坡带 ,稳定型水下扇主要发育在扇三角洲的前端 ,气候因素也为稳定型水下扇形成创造了物源条件 ;基准面升降影响着水下扇的相序特征 ,低水位体系域和水退体系域易形成推进型水下扇 ,水进体系域易形成退缩型水下扇 ;半深湖 -深湖的滞水条件是水下扇得以保存的前提。统计结果表明本区获工业油气流的井主要集中在中扇 ,其中辫状水道微相最为富集。
    Abstract: It is typically developed lacus subaqueous fan of Shuangyang Formation in Moliqing fault subsidence of Yitong Basin in Eocene. According to core, well-logging and seismic data, associated with grading analysis and other methods, lacus subaqueous fan is divided into inner fan, middle fan and out fan. From bottom to top a integrated prograding lacus subaqueous fan is consisted of out fan, middle fan and inner fan subfacies in vertical , and it has the features that show thicker, coarser towards up. Inner fan can be further separated into channel, channel levee and slump deposits, middle fan is classified into braided channel, braided interchannel and suppafan lobes, and out fan is consisted of classic turbidites and lacustrine mudstone. Subaqueous fan is mainly formed at the side of steep slope controlled by contemporary fault, and some formed at the front of fan-delta. Primary factors which influence the distribution and emergence of subaqueous fan is that movements of contemporary fault bring steep landform, episode movements of which make up of the burst mechanics of subaqueous gravity flow forming. Subaqueous fan of steep slope mainly occurs at the zone of steep slope, stable subaqueous fan mostly emerges at the front of fan-delta, meanwhile climate is a favorable factor for stable subquous fan. Base-level affects the features of facies orders. It is easily formed prograding subaqueous fan in lowstand systems tracts and regressive systems tracts, there develop regressive subaqueous fan in the transgressive systems tracts as well. The precondition that preserves subaqueous fan is the backwater environment of deeper or deep lacus. The results of statistics show that all that bear industrial petroleum and gas mostly concentrated in the middle fan, and of which is much rich in the braided channel.
    • HTML全文
    • 参考文献(1)
  • [1] ［1］Gorsline D S, Emery K O. Turbidity current deposits in San Pedro and Santa Monica basins of southern California[J]. Geol Soc America Bull, 195 9, 70:279～290

    ［2］Sullwold H H, Jr. Tarzana fan-deep submarine fan of late Miocene age, Los Angeles County, California[J]. AAPG Bull, 1960,44:433～457

    ［3］Jacka A D, et al. Permian deep-sea fans of the Delaware mountain gr oup (Guadalupian), Delaware basin[J]. Soc Econ Paleontol Mineral Permian, Basi n Section Publ, 1968, 68～11: 49～90

    ［4］Walker R G. Deep-water sandstone facies and ancient submarine fans: Mo dels for exploration for stratigraphic traps[J]. AAPG Bull,1978, 62:932～966

    ［5］Bauma A H, Normark W R, Barnes N E. Submarine fans and related turbidit e systems[M]. New York: Springer-Verlag, 1985. 351

    ［6］Shanmugam G, Moiola R G. Submarine fans: characteristics, models, class ification, and reservoir potential[J]. Earth Sciences Review,1988,24:383～428

    ［7］刘招君,王东坡,何起祥. 攀西地区上三叠统湖泊浊积岩沉积特征及其地质意义 [A]. 见:张云湘主编. 中国攀西裂谷文集[C]. 北京:地质出版社,1985.298～306[Li u Zhaojun, Wang Dongpo, He Qixiang. Sedimentary Character and Geological Signifi cance of Upper Triassic Lake Facies Turbidite in Panxi Area[A].In:Zhang Yunxia ng, ed. Contribution to Panxi Rift China[C].Beijing: Geological Publishing Hou se,1985.198～306]

    ［8］吴崇筠,李纯菊,等. 断陷盆地中的浊积岩[A]. 见:中国石油学会石油地质委员会主编. 碎屑岩沉积相研究[C].北京:石油工业出版社,1988. 1～17[Wu Chongyun, L i Chunju, et al. Turbidite in faulted subdidence-lake basin[A]. In:Petrol eum Geology Institute of Chinese Petroleum Society, ed. Study of Clastic Sedim entary Facies[C].Beijing: Petroleum Industry Press,1988.1～17]

    ［9］丘东洲,何治亮. 陆盆扇体沉积的形成机制及其油气意义[A]. 见:中国石油学会石油地质委员会主编. 碎屑岩沉积相研究[C].北京:石油工业出版社,1988.148～154[ Qiu Dongzhou,He Zhiliang.Oil and Gas Reservoir in Continental Basin[A]. In:Pet roleum Geology Institute of Chinese Petroleum Society, ed. Study of Clastic S edimentary Facies[C]. Beijing: Petroleum Industry Press,1988.148～154]

    ［10］Allen P A and Allen J R. Basin analysis: principles and applications: Blackw ell Scientific Publications[C]. Oxford, London. 1990

    ［11］Posamentier H W and Vail P R. Eustatic controls on clastic deposition Ⅱ-Se quence and systems tract models[A]. In: Wilgus C K, et al, eds. Sea-level changes: an inlegrated approach[C]. SEPM Special Publication, 1988, 42:125～15 4

    ［12］刘招君,董清水,王嗣敏等. 陆相层序地层学导论与应用[M]. 北京:石油工业出版社,2002[Liu Zhaojun, Dong Qingshui, Wang Siming, et al. Introduction to Cont inental Sequence Stratigraphy & Application[M]. Beijing: Petroleum Industry P ress, 2002]

    ［13］Van Wagoner J C, et al. Siliciclastic sequence stratigraphy, in well log s, cores and outcrops: concepts for High-Resolution Correlation of Time and Fac ies[M]. Published by the American Association of Petroleum Geologists. Oklaho ma, USA, 1990
    • 相关文章
  • [1] 刘海, 徐耀辉, 李阳, 黄凌松, 吕奇奇, 刘忠保.  海陆过渡相三角洲沉积体系陆源有机质沉积特征及其影响因素的模拟实验研究 . 沉积学报, 2024, 42(1): 251-265. doi: 10.14027/j.issn.1000-0550.2023.047
    [2] 杨仁超, 李作福, 张学才, 慈兴华, 方旭庆, 李传华, 刘海宁.  异重流沉积研究进展与展望 . 沉积学报, 2023, 41(6): 1917-1933. doi: 10.14027/j.issn.1000-0550.2023.008
    [3] 刘晶晶, 毛毳, 刘兴瑀, 魏荷花, 权莲顺, 刘泽璇, 张文鑫, 赵冰, 张青.  钙华的形成环境与特征及在油气储集方向的探讨 . 沉积学报, 2021, 39(6): 1425-1439. doi: 10.14027/j.issn.1000-0550.2021.124
    [4] 谷渊涛, 李晓霞, 万泉, 杨曙光.  泥页岩有机质孔隙差异特征及影响因素分析 . 沉积学报, 2021, 39(4): 794-810. doi: 10.14027/j.issn.1000-0550.2020.134
    [5] 黄文奥, 赵晓明, 谭程鹏, 葛家旺, 冯双奇, 李晨曦, 陆文明.  西秦岭直合隆地区三叠系深水水道沉积模式分析 . 沉积学报, 2020, 38(5): 1061-1075. doi: 10.14027/j.issn.1000-0550.2019.097
    [6] 屈童, 高岗, 徐新德, 刘凤妍.  三角洲—浅海沉积体系陆源有机质分布控制因素 . 沉积学报, 2020, 38(3): 648-660. doi: 10.14027/j.issn.1000-0550.2019.057
    [7] 赵迪斐, 郭英海, WangGeoff, 李冠霖, 曾春林, 焦伟伟.  层序地层格架及其对页岩储层发育特征的影响-以四川盆地龙马溪组页岩为例 . 沉积学报, 2020, 38(2): 379-397. doi: 10.14027/j.issn.1000-0550.2019.043
    [8] 孙志峰, 林承焰, 董春梅.  复杂曲流带识别标志及其内部点坝叠加接触模式 . 沉积学报, 2018, 36(2): 366-375. doi: 10.14027/j.issn.1000-0550.2018.023
    [9] 田庆春, 杨太保, 石培宏.  可可西里古湖泊沉积物有机碳δ13C变化特征及其影响因素 . 沉积学报, 2016, 34(2): 260-267. doi: 10.14027/j.cnki.cjxb.2016.02.005
    [10] 黄薇, 吴海波, 李军辉, 刘赫.  海—塔盆地中部断陷带南屯组沉积体系配置及有利相带分析 . 沉积学报, 2016, 34(1): 120-128. doi: 10.14027/j.cnki.cjxb.2016.01.011
    [11] 张辉, 王怀厂, 刘新社, 赵会涛.  古湖岸线确定及其对优质储集层控制——以鄂尔多斯盆地北部地区盒8段为例 . 沉积学报, 2015, 33(2): 348-356. doi: 10.14027/j.cnki.cjxb.2015.02.014
    [12] .  沉积物岩芯X光片图像灰度数值及其影响因素 . 沉积学报, 2012, 30(2): 318-324.
    [13] 齐红艳.  长江口及邻近海域表层沉积物pH、Eh分布及制约因素 . 沉积学报, 2008, 26(5): 820-827.
    [14] 魏垂高 张世奇 姜在兴 刘金华.  东营凹陷现河地区沙三段震积岩特征及其意义 . 沉积学报, 2006, 24(06): 798-805.
    [15] 杨占龙, 郭精义, 陈启林, 宋广寿, 黄刚.  银根盆地查干凹陷火山沉积岩岩相特征及其识别标志 . 沉积学报, 2005, 23(1): 67-72.
    [16] 杨剑萍, 王辉, 陈世悦, 袁静, 鄢继华, 赵卫卫.  济阳坳陷古近系震积岩特征 . 沉积学报, 2004, 22(2): 281-287.
    [17] 张在龙, 许国梁, 叶天旭, 蔺五正, 劳永新.  天然矿物存在下脂肪酸酯水解生烃的影响因素研究 . 沉积学报, 2003, 21(4): 717-721.
    [18] 张发强, 王震亮, 吴亚生, 杨计海, 罗晓容.  消除影响压实趋势线地质因素的方法——以莺歌海盆地为例 . 沉积学报, 2002, 20(2): 326-332.
    [19] 胡受权, 郭文平, 杨凤根, 颜其彬, 刘树根, 童崇光.  试论控制断陷湖盆陆相层序发育的影响因素 . 沉积学报, 2001, 19(2): 256-262.
    [20] 张德玉.  马里亚纳海槽和西菲律宾海盆更新世以来沉积物中的粘土矿物 . 沉积学报, 1993, 11(1): 111-120.
    • 施引文献
  • 资源附件(0)
  • 加载中
WeChat 点击查看大图
计量
  • 文章访问数:  638
  • HTML全文浏览量:  6
  • PDF下载量:  501
  • 被引次数: 0
出版历程
  • 收稿日期:  2002-12-26
  • 修回日期:  2003-01-10
  • 刊出日期:  2003-03-10

目录

    湖泊水下扇沉积特征及影响因素——以伊通盆地莫里青断陷双阳组为例

    • 吉林大学地球科学学院 长春130061
    • 收稿日期: 2002-12-26
    • 修回日期: 2003-01-10
    • 刊出日期: 2003-03-10

    • 中图分类号: P512.2

    摘要: 伊通盆地莫里青断陷始新统双阳组发育典型的湖泊水下扇体。根据岩心、测井和地震资料 ,并结合粒度分析等方法 ,将其划分为内扇、中扇和外扇亚相及某干微相。影响水下扇形成和分布的主要因素是 :同生断裂的活动造就了陡坡地形 ,其幕式活动成为水下扇形成的触发机制 ;阵发型水下扇主要发育在陡坡带 ,稳定型水下扇主要发育在扇三角洲的前端 ,气候因素也为稳定型水下扇形成创造了物源条件 ;基准面升降影响着水下扇的相序特征 ,低水位体系域和水退体系域易形成推进型水下扇 ,水进体系域易形成退缩型水下扇 ;半深湖 -深湖的滞水条件是水下扇得以保存的前提。统计结果表明本区获工业油气流的井主要集中在中扇 ,其中辫状水道微相最为富集。

    English Abstract

    刘招君. 湖泊水下扇沉积特征及影响因素——以伊通盆地莫里青断陷双阳组为例[J]. 沉积学报, 2003, 21(1): 148-154.
    引用本文: 刘招君. 湖泊水下扇沉积特征及影响因素——以伊通盆地莫里青断陷双阳组为例[J]. 沉积学报, 2003, 21(1): 148-154.
    shu
    LIU Zhao-jun. Lacus Subaqueous Fan Sedimentary Characteristics and Influence Factors——A Case Study of Shuangyang Formation in Moliqing Fault Subsidence of Yitong Basin[J]. Acta Sedimentologica Sinica, 2003, 21(1): 148-154.
    Citation: LIU Zhao-jun. Lacus Subaqueous Fan Sedimentary Characteristics and Influence Factors——A Case Study of Shuangyang Formation in Moliqing Fault Subsidence of Yitong Basin[J]. Acta Sedimentologica Sinica, 2003, 21(1): 148-154.
    shu

      全文HTML

    参考文献 (1)

    目录

      /

      返回文章
      返回

      友情链接

      期刊在线

      联系我们

      • 网站版权 © 2011《沉积学报》编辑部
      • 地址: 兰州市天水中路8号
      • 邮编: 730000   Tel:（0931）8264231
      • 陇ICP备2021001824号-28
      • 甘公网安备 62010202000673号
      关注微信公众号

      Email alert

      RSS

      系统由 北京仁和汇智信息技术有限公司 设计集成    百度统计

      x 关闭 永久关闭

      2023年地质事件沉积研究新进展国际学术研讨会（第一号通知）