QIN Jianxiong, ZENG Yongfu, CHEN Hongde, TIAN Jingchun. SEQUENCE STRATIGRAPHY STUDY OF CARBONATE SLOPE DEPOSIT[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1999, 21(2): 110-118. doi: 10.11781/sysydz199902110
Citation: QIN Jianxiong, ZENG Yongfu, CHEN Hongde, TIAN Jingchun. SEQUENCE STRATIGRAPHY STUDY OF CARBONATE SLOPE DEPOSIT[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1999, 21(2): 110-118. doi: 10.11781/sysydz199902110

SEQUENCE STRATIGRAPHY STUDY OF CARBONATE SLOPE DEPOSIT

doi: 10.11781/sysydz199902110
  • Received Date: 1998-05-21
  • Publish Date: 1999-04-25
  • Study on the Permian Sequence Stratigraphy of the Youjiang Basin reveals that gravity flow develops during every period of eustatic cycles and it displays individual characteristic internal configuration and genetic framework of sequences.Lowstand is characterized by basin margin-downslope miscellaneous lithic turbidites,and gravity flow is relatively less in shelf marginal systems.During transgressive periods,gravity flow is dominated by calcarenaceous clastic flow and its recomposed sand deposit.The deposit of gravity flow in highstand has large thickness,wide distribution and rich genetic patterns,and is mainly characterized by well-developed calcarenaceous colluvial rocks,grain flow,liquefied sediment flow,clastic flow,and turbidity flow.

     

  • loading
  • [1]
    Walder R G et al.Facies Models-Response to sea level change.Geological Association of Canada.1992:349~374
    [2]
    Cook H E.Carbonafe-slope failures as indicators of sea level lowerings.AAPG,1991,75(5):566(abstract)
    [3]
    Tose L A.Sequence stratigraphy of mixed carbonate/volcaniclastic slope deposits flanking the Scilicar-Catinaccio Buileup,Dolomites,Italy.In Bradnex R,The northern margin of the Catinaccio Platform,Guide-book Excursion A,1991:17~39
    [4]
    Grammer G M et al.Highstand versus lowstand deposition on carbonate platform margins:insight from Quaternary foreslopes in the Bahamas.Marine Geology,1992,103(1):125~136
    [5]
    Glaser k s et al.High production and highstand shedding from deeply submerged carbonate banks,northern Nicarahuan Rise.Journal of Sedimentary Petrology,1991,61(2):128~142
    [6]
    Chiocci F L.Effect of sea-level variation on upper-slope depositional processes offshore of Tiber delta,Italy.Marine Geology,1992,104(2):109~122
    [7]
    Trincardi F.Collapse and flow of lowstand shelf-margin deposits:An example from the eastern Tyrrhenian Sea,Marine Geology,1992,105(4):77~94
    [8]
    Steinhauff D M.Recognizing exposure,drowning,and "missing beats":platform-interior to platform-margin seqnence stratigraphy of middle Ordovician,east Tennessee.Journal of Sedimentary Research,1995,65(2):183~207
    [9]
    Melim L A et al.The forereef facies of the Permian Caption Formation:Therole of sediment supply versus sea-level change.Journal of Sedimentary Research,1995,65(1):107~118
    [10]
    Schlager W.Submarine slipe angles,drowning unconformities,and selferosion of limestone escarpments.Geology,1986,14(1):726~765
    [11]
    Masetti D.Deep-water asymmetric cycles and progradation of carbonate platforms governed by high-frequency eustatic ationsoscill.Geology,1991,79(7):336~339
    [12]
    Mullins H T et al.Three-dimensional sedimentary fromeword of central west Florida:A sequential seismic stratigraphic perspective.Geological Society of America,Bulletin,1988,100(4):514~538
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Article Metrics

    Article views (576) PDF downloads(449) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return