Advanced Search

Indexed by SCI、CA、РЖ、PA、CSA、ZR、etc .

Volume 23 Issue 4
Aug 2012
Turn off MathJax
Article Contents
Hao Li, Changsong Lin, Yanmei Zhang, Rongxi Zhang, Zhifeng Rui, Lili Huang. Stratigraphic Architecture and Computer Modelling of Carbonate Platform Margin, Late Ordovician Lianglitage Formation, Central Tarim Basin. Journal of Earth Science, 2012, 23(4): 627-638. doi: 10.1007/s12583-012-0279-9
Citation: Hao Li, Changsong Lin, Yanmei Zhang, Rongxi Zhang, Zhifeng Rui, Lili Huang. Stratigraphic Architecture and Computer Modelling of Carbonate Platform Margin, Late Ordovician Lianglitage Formation, Central Tarim Basin. Journal of Earth Science, 2012, 23(4): 627-638. doi: 10.1007/s12583-012-0279-9

Stratigraphic Architecture and Computer Modelling of Carbonate Platform Margin, Late Ordovician Lianglitage Formation, Central Tarim Basin

doi: 10.1007/s12583-012-0279-9
Funds:

the Frontier Research Project of Marine Facies of the Oil Industry in China and the National Basic Research Program of China 2011CB201100-03

the Frontier Research Project of Marine Facies of the Oil Industry in China and the National Basic Research Program of China 2006CB202302

the National Natural Science Foundation of China 41130422

the National Natural Science Foundation of China 40372056

More Information
  • Corresponding author: Hao Li, lihao11909@163.com
  • Received Date: 05 Mar 2012
  • Accepted Date: 20 May 2012
  • Publish Date: 01 Aug 2012
  • According to the different geometries and reflected characteristics in the seismic sections,the carbonate platform margin of the northern slope can be summarized as three basic depositional architectures in the Late Ordovician Lianglitage (良里塔格) Formation of the Tazhong (塔中) uplift. The type one mainly located in the west of the carbonate platform margin,and it showed obvious imbricate progradation from the interior to the margin of the platform. The type two was in the middle of the carbonate platform margin,which showed retrogradational stacking pattern in the same transgressive systems tract period,and the slope strata of the platform margin showed progradational sequence in the highstand systems tract period. The type three located in the east of the carbonate platform margin,and it showed the parallel aggradational architecture. The crossing well section along the northern slope of the Tazhong carbonate platform showed that the depositional thickness became thinner from the east to the west. The thickest belt located in the east of the platform margin,and became thinner rapidly towards the basin and the platform interior. These indicated that the paleogeomorphology of the Tazhong uplift was probably high in the west and low in the east during the period of the Late Ordovician Lianglitage Formation. According to the interpretation of seismic profiles and the computer modelling result,the depositional architectures of sequence O3 l-2 showed aggradation,retrogradation and progradation from the east to the west of the carbonate platform margin during the transgression period. This meant that the accommodation became smaller gradually from the east to the west along the northern carbonate platform margin of the Tazhong uplift. The difference of the accommodation was probably caused by the difference of tectonic subsidence. Also,computer-aided modelling can be used to deeply understand the importance of various control parameters on the carbonate platform depositional architectures and processes.

     

  • loading
  • Aurell, M., Bosence, D., Waltham, D., 1995. Carbonate Ramp Depositional Systems from a Late Jurassic Epeiric Platform (Iberian Basin, Spain): A Combined Computer Modelling and Outcrop Analysis. Sedimentology, 42(1): 75–94 doi: 10.1111/j.1365-3091.1995.tb01272.x
    Bice, D., 1988. Synthetic Stratigraphy of Carbonate Platform and Basin Systems. Geology, 16: 703–706 doi: 10.1130/0091-7613(1988)016<0703:SSOCPA>2.3.CO;2
    Bitzer, K., 1996. Modeling Consolidation and Fluid Flow in Sedimentary Basins. Computers & Geosciences, 22(5): 467–478 http://www.onacademic.com/detail/journal_1000034995744010_6ba8.html
    Bitzer, K., 1999. Two-Dimensional Simulation of Clastic and Carbonate Sedimentation, Consolidation, Subsidence, Fluid Flow, Heat Flow and Solute Transport during the Formation of Sedimentary Basins. Computer & Geosciences, 25(4): 431–447 http://onlinelibrary.wiley.com/resolve/reference/ADS?id=1999CG.....25..431B
    Bosence, D. W. J., 1989. Biogenic Carbonate Production in Florida Bay. Bull. Mar. Sci. , 44: 419–433
    Bosence, D. W. J., Waltham, D. A., 1990. Computer Modelling the Internal Architecture of Carbonate Platforms. Geology, 18: 26–30 doi: 10.1130/0091-7613(1990)018<0026:CMTIAO>2.3.CO;2
    Eberli, G. P., Masaferro, J. L., Sarg, J. F., et al., 2004. Seismic Imaging of Carbonate Reservoirs and Systems. AAPG Memoir, 81: 207–250 http://www.openisbn.com/download/0891813624.pdf?name=Seismic_Imaging_Of_Carbonate_Reservoirs_And_System
    He, D. F., Jia, C. Z., Li, D. S., et al., 2005. Formation and Evolution of Polycyclic Superimposed Tarim Basin. Oil & Gas Geology, 26(1): 64–77 (in Chinese with English Abstract) http://www.cnki.com.cn/Article/CJFDTotal-SYYT200501009.htm
    Jia, C. Z., 1997. Tectonic Characteristics and Petroleum in Tarim Basin of China. Petroleum Industry Press, Beijing (in Chinese)
    Lin, C. S., Erikoson, K., Li, S. T., et al., 2001. Sequence Architecture, Depositional Systems, and Controls on Development of Lacustrine Basin Fills in Part of the Erlian Basin, Northeast China. AAPG Bulletin, 85(11): 2017–2043
    Lin, C. S., Li, S. T., Zhang, Q. M., et al., 1997. Lithospheric Stretching, Subsidence and Thermal History Modelling: Application to Yinggehai, Qiongdongnan and Songliao Basins in East China. Journal of China University of Geosciences, 8(1): 83–89
    Lin, C. S., Yang, H. J., Liu, J. Y., et al., 2008. Early Paleozoic Paleo-Uplift Geomorphology of Tarim Basin and Development and Distribution of Tectomic Palaeogeography and Formation Trap. Oil & Gas Geology, 29(2): 189–197 (in Chinese with English Abstract)
    Lin, C. S., Yang, H. J., Liu, J. Y., et al., 2009. Paleostructural Geomorphology of the Paleozoic Central Uplift Belt and Its Constraint on the Development of Depositional Facies in the Tarim Basin. Science in China (Series D), 39(3): 306–316 (in Chinese)
    Lin, C. S., Zhang, Y. M., Li, S. T., et al., 1996. Sequence Stratigraphy Modelling of Sedimentary Basin: Conceptual Model and Application to Erlian and Yinggehai Basins. Journal of China University of Geosciences, 7(1): 132–137 http://www.cqvip.com/main/none.aspx?lngid=3001187748
    Lin, C. S., Zhang, Y. M., Li, S. T., et al., 2002. Quantitatively Modelling of Multiple Stretching of Lithosphere and Deep Thermal History of Some Tertiary Rift Basins in East China. Acta Geol. Sin. , 76(3): 324–330
    Marion, D., Jizba, D., 1997. Acoustic Properties of Carbonate Rocks: Use in Quantitative Interpretation of Sonic and Seismic Measurements Series. In: Palaz, I., Marfurt, K. J., eds., Carbonate Seismology. Society of Exploration Geophysicists, Tulsa. 75–94
    Morsilli, M., Rusciadelli, G., Vichi, G., et al., 2000. Gravity-Driven Processes: Control on Margin Architecture and Slope Evolution in a Cretaceous Carbonate Platform (Montagna Della Maiella, Italy). AAPG International Conference and Exhibition, 84: 1467 doi: 10.1306/a9674af8-1738-11d7-8645000102c1865d
    Schlager, W., 1992. Sedimentology and Sequence Stratigraphy of Reefs and Carbonate Platforms. AAPG Continuing Education Course Note Series, 34: 1–10
    Schlager, W., 2000. The Future of Applied Sedimentology. Journal of Sedimentary Research, 70(1): 2–9 doi: 10.1306/2DC408F8-0E47-11D7-8643000102C1865D
    Schlager, W., 2005. Carbonate Sedimentology and Sequence Stratigraphy (SEPM Concepts in Sedimentology & Paleontology 8). Free Univ., Amsterdam. 72
    Tipper, J. C., 1997. Modeling Carbonate Platform Sedimentation-Lag Comes Maturally. Geology, 25(6): 495–498 doi: 10.1130/0091-7613(1997)025<0495:MCPSLC>2.3.CO;2
    Williams, T., Kroon, D., Spezzaferri, S., 2002. Middle and Upper Miocene Cyclostratigraphy of Downholelogs and Short to Long Term Astronomical Cycles in Carbonate Production of Great BahamaBank. Marine Geology, 185(1–2): 75–93 http://www.sciencedirect.com/science/article/pii/S0025322701002912
  • 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

    Figures(9)

    Article Metrics

    Article views(928) PDF downloads(26) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return