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Li Sitian. Current Review of Sedimentary Basin Analysis[J]. Acta Sedimentologica Sinica, 1992, 10(3): 10-15.
Citation: Li Sitian. Current Review of Sedimentary Basin Analysis[J]. Acta Sedimentologica Sinica, 1992, 10(3): 10-15.

Current Review of Sedimentary Basin Analysis

  • Publish Date: 1992-09-10
  • Sequence stratigraphy, an important and significant development in sedimentology and stratigraphy, has made the sedimentary basin filling analysis both theoretical and methodological. Setting up the chronstratigraphic framework and determinging the building blocks have: now become the major'tasks in basin analysis. This paper describes the rapid development in sequence stratigraphy and its relationship with other subjects such as depositional system analysis, tectono-stratigraphy and event stratigraphy. The inter-relationship among these subjects will become the basis for a new genetic stratigraphy system that centents the sequence stratigraphy. This system will strongly support the research in sedimentay basin anaiysis. Studies in sandbody architectural units, the basis for sedimentology of oil reservoir is also part of the research in building blocks of basin filling. This paper discussed the construction of sequence stratigraphic models for various basins, especially the intraplate paralic basins and the inland basius, both being the major types in China. The paper also discusses problems in theoretical research in China related to sequence stratigraphy, suggestions are as follows: 1. Based upon the sedimentology, micropaleontology and magnetostratigraphy research of the South China sea basis and East China sea basin, the Cenozoic sea level changes scheme could be constructed firstly, also the generalized schemes of sea level changes of the other periods in mainland could be put forward. 2.There are optimum conditions for the studies of Paleozoic seqquence stratigraphy from intracontinent to continent margin of the Yangtze and Sino-Korean cratons. 3. Mesozoic and Cenozoic inland basins cover vast area of China continent. To strudy sequence stratigraphy in the lacustrine basins is of great significance, and the indirect efficacy of sea level changes to lacustrine basin may be a key problem. Tectonism has great influence on the extensional and flexural basins in the continental area so tectono-stratigraphy analysis has more importance in the basin research.
  • [1] (1) 新妻信明,1986,东北日本孤四地质构造发达、本朝彦、中村一明编日本列岛之形成,253-265页.

    (2) Heck R. A. et al. 1988, Geological Sociaty of America Memoir 171,p,. 456 -487.

    (3) Brown L.F., and W. L. Fisher, 1977, AAPG Memoir 26. p.213-248

    (4) Haq B. U. et al., 1988, Mesozoic and Cenozoic chronostratigraphy and cycles of sea-level change, in: Sea LevelChanges-An Integrated Approach. SEPM Special Publication No.42

    (5) Kauffman L. G.。1988. Concepts and methods of high-resolution event stratigraphy, Ann. Rev. Earth Planet Sci.16

    (6) Lawrence D. T·M.Doyle T. Aigner 1990, AAPCi Bulletin, V.74, N.3, p.273-295

    (7) Miall. A. D. 1985, Earth Sci. Rev., 22, p.261-308

    (8) Maill, A. D. 1989. Architectural elements and bounding Surfaces in channelized elastic deposits: notes on compari-sons between Iluvial and furbidite systems, in: A. Taira and F. Masuda Sedimentary Facies in the Active Plate Mar-gm, 3-15

    (9) Steel R. J.,1988, Coarsening- upward and skewed fan bodies: sympotems of strike- slipp and transfer faultmovement in sedimentary basins, in: Fan Deltas: Sedimentology and Tectonic Settings, p.75-83

    (10) TankaEd A. J., 1986, AAPG Bulletin V.70. N.7, p.853-868

    (12) Tokuhashi, S, 1989,Two stages ot'submarine fan sedimentation in an ancient forearc basin, central Japan, In A.Taira and F.Masuda, Sedimentary Facies in the Active Plate Margin, p.439-468

    (12) Vail P. R. et al.,1990. The Stratigraphic Signatures of Tectonics, eustasy and Sedimentation-an Overview Department of Geology and Geophysics. Rice University Houston Texas Version p90-917

    (13) Vail, P. R. et al., 1977. Seismic stratigraphy and global changes of sea level, Part 3: relative changes of sea levelfram coastal onlap, in: C. W.Payton (ed),Seismic stratigraphy applications to hydrocarbon exploration: AAPG Memoir 26, p.63-97

    (14) Van Wagoner J.C.et al, 1990, Siliciclastic Sequence Stratigraphy in Well Logs. Cores, and Outcrops: Concepts for High-Resolution Correlation of Time and Fades, AAPG Methods in Exploration Series, No.7
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  • Published:  1992-09-10

Current Review of Sedimentary Basin Analysis

Abstract: Sequence stratigraphy, an important and significant development in sedimentology and stratigraphy, has made the sedimentary basin filling analysis both theoretical and methodological. Setting up the chronstratigraphic framework and determinging the building blocks have: now become the major'tasks in basin analysis. This paper describes the rapid development in sequence stratigraphy and its relationship with other subjects such as depositional system analysis, tectono-stratigraphy and event stratigraphy. The inter-relationship among these subjects will become the basis for a new genetic stratigraphy system that centents the sequence stratigraphy. This system will strongly support the research in sedimentay basin anaiysis. Studies in sandbody architectural units, the basis for sedimentology of oil reservoir is also part of the research in building blocks of basin filling. This paper discussed the construction of sequence stratigraphic models for various basins, especially the intraplate paralic basins and the inland basius, both being the major types in China. The paper also discusses problems in theoretical research in China related to sequence stratigraphy, suggestions are as follows: 1. Based upon the sedimentology, micropaleontology and magnetostratigraphy research of the South China sea basis and East China sea basin, the Cenozoic sea level changes scheme could be constructed firstly, also the generalized schemes of sea level changes of the other periods in mainland could be put forward. 2.There are optimum conditions for the studies of Paleozoic seqquence stratigraphy from intracontinent to continent margin of the Yangtze and Sino-Korean cratons. 3. Mesozoic and Cenozoic inland basins cover vast area of China continent. To strudy sequence stratigraphy in the lacustrine basins is of great significance, and the indirect efficacy of sea level changes to lacustrine basin may be a key problem. Tectonism has great influence on the extensional and flexural basins in the continental area so tectono-stratigraphy analysis has more importance in the basin research.

Li Sitian. Current Review of Sedimentary Basin Analysis[J]. Acta Sedimentologica Sinica, 1992, 10(3): 10-15.
Citation: Li Sitian. Current Review of Sedimentary Basin Analysis[J]. Acta Sedimentologica Sinica, 1992, 10(3): 10-15.
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