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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

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.
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.

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

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

  • 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。
  • [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
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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

    • 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.
    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.
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