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CHEN Hong de, QIN Jian xiong, TIAN Jing chun, PENG Jun, HOU Zhong jian. Sequence Filling Dynamics of Youjiang Basin,Southern China[J]. Acta Sedimentologica Sinica, 2000, 18(2): 165-171.
Citation: CHEN Hong de, QIN Jian xiong, TIAN Jing chun, PENG Jun, HOU Zhong jian. Sequence Filling Dynamics of Youjiang Basin,Southern China[J]. Acta Sedimentologica Sinica, 2000, 18(2): 165-171.

Sequence Filling Dynamics of Youjiang Basin,Southern China

  • Received Date: 1999-06-30
  • Publish Date: 2000-06-10
  • In the light of sequence-basin-earth theory in conjunction with previou s stra tigraphy,sedimentology,basin analysis and sequence stratigraphy,the sequence fil ling dyna mics of Youjiang Basin has been studied in detail.Fi ve hierachies of sequence boundaries and corresponding five hierachies of deposi tional sequences,1 super-order sequence,4 1st-order sequences,6 2nd-order sequen ces,11 sequence sets,47 3rd-order sequences and a certain amount of 4th-and 5th- order seq uences have been recognized for the first time.Relationship between sequence bo un dary and geological events,and that of sequence hierachy and basin type have bee n discusse d,and then sequence stratigraphic framework of Youjiang Basin has also been established.By the cognition that sequence development of rifting basin is mai nly controlled by synsedimentary fault and fundamental subsidence,relationship b etween sequence genesis and basin structure has been set up. The sequence f ramework and filling proccess are obviously distinct within different genetic ba sins. Finally,the author delibr ated the sequence filling dynamic process and related basin evolution of the You jiang Basin.On the basis of the research result mentioned above,this paper sugg e sts that the sequence filling process of the Youjiang Basin can be subdivided in to four stages:intracontinental rifting,marginal rifting,retroarc rifting and fo reland basin,constituting a complete tectonic cycles during Hercynian-In dosinian stage.
  • [1] 曾允孚,刘文均.华南右江盆地沉积构造演化[M] .北京:地质出版社, 1993.1~96
    [2] 陈洪德,曾允孚.右江沉积盆地的性质及演化讨论[J] .岩相古地理,1990.1 1(1):28~37
    [3] 秦建华,吴应林,颜仰基等.南盘江盆地海西-印支期沉积构造演化[J] .地 质学报,1996,70(2):99~107
    [4] Krapez B.Sequence stratigraphic concepts applied to the identificatio n of depositional basins and global tectonic cycles[J] .Austailian Journal of Ear th Sciences,1997,(44):1~36
    [5] 陈代钊,陈其英.华南泥盆纪沉积演化及海水进退规程[J] .地质科学,29(3) :246~255
    [6] 王鸿祯,史晓颖.沉积层序及海平面旋回的分类级别[J] .现代地质,1998,1 2(1):1~16
    [7] Shanmugam G.Origin,recognition,and importance of erosional unconformit ies in sedimentary basin[A] .In:Kleinspehn K L, Paola C, ed,New Perspectives in Ba sin Analysis[C] .Springer-Verlag,New York,1998.83~108
    [8] Galloway W E.Genetic stratigraphic sequences in basin analysis Ⅰ:Arch it ecture and genesis of flooding-surface bounded depositional units[J] .AAPG,73( 2):125~142
    [9] Krapez B.Sequence stratigraphic concepts applied to the identification of basin-filling rhythms in Precambrian successions[J] .Australian Journal of E arth Sciences.1993,(43):355~380
    [10] Brett C E,Goodman M W,LoDuca S T.Sequence,cycle and basin dynamics in theSillurian of the Appalachian Foreland Basin[J] .Sedimentary Geology,1990,6 9:191~224
    [11] Ross C A,Ross J R.Late Paleozoic sea level and depositional sequenc e[A] .Cushman Foundation for Forminiferal Research,Special Publication.1987.24 ~137
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  • Received:  1999-06-30
  • Published:  2000-06-10

Sequence Filling Dynamics of Youjiang Basin,Southern China

Abstract: In the light of sequence-basin-earth theory in conjunction with previou s stra tigraphy,sedimentology,basin analysis and sequence stratigraphy,the sequence fil ling dyna mics of Youjiang Basin has been studied in detail.Fi ve hierachies of sequence boundaries and corresponding five hierachies of deposi tional sequences,1 super-order sequence,4 1st-order sequences,6 2nd-order sequen ces,11 sequence sets,47 3rd-order sequences and a certain amount of 4th-and 5th- order seq uences have been recognized for the first time.Relationship between sequence bo un dary and geological events,and that of sequence hierachy and basin type have bee n discusse d,and then sequence stratigraphic framework of Youjiang Basin has also been established.By the cognition that sequence development of rifting basin is mai nly controlled by synsedimentary fault and fundamental subsidence,relationship b etween sequence genesis and basin structure has been set up. The sequence f ramework and filling proccess are obviously distinct within different genetic ba sins. Finally,the author delibr ated the sequence filling dynamic process and related basin evolution of the You jiang Basin.On the basis of the research result mentioned above,this paper sugg e sts that the sequence filling process of the Youjiang Basin can be subdivided in to four stages:intracontinental rifting,marginal rifting,retroarc rifting and fo reland basin,constituting a complete tectonic cycles during Hercynian-In dosinian stage.

CHEN Hong de, QIN Jian xiong, TIAN Jing chun, PENG Jun, HOU Zhong jian. Sequence Filling Dynamics of Youjiang Basin,Southern China[J]. Acta Sedimentologica Sinica, 2000, 18(2): 165-171.
Citation: CHEN Hong de, QIN Jian xiong, TIAN Jing chun, PENG Jun, HOU Zhong jian. Sequence Filling Dynamics of Youjiang Basin,Southern China[J]. Acta Sedimentologica Sinica, 2000, 18(2): 165-171.
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