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Volume 15 Issue 1
Mar 2004
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Mingxiang Mei, Yongsheng Ma, Jun Deng, Qingfen Meng, Dinghong Yi, Donghai Li. Late Paleozoic Sequence-Stratigraphic Frameworks and Sea Level Changes in Dianqiangui Basin and Its Adjacent Areas with Systematic Revision of Regional Unconformities. Journal of Earth Science, 2004, 15(1): 55-68.
Citation: Mingxiang Mei, Yongsheng Ma, Jun Deng, Qingfen Meng, Dinghong Yi, Donghai Li. Late Paleozoic Sequence-Stratigraphic Frameworks and Sea Level Changes in Dianqiangui Basin and Its Adjacent Areas with Systematic Revision of Regional Unconformities. Journal of Earth Science, 2004, 15(1): 55-68.

Late Paleozoic Sequence-Stratigraphic Frameworks and Sea Level Changes in Dianqiangui Basin and Its Adjacent Areas with Systematic Revision of Regional Unconformities

Funds:

the China Petrochemical Corporation (SINOPEC) 

  • Received Date: 10 Nov 2003
  • Accepted Date: 25 Dec 2003
  • The formation process of the Dianqiangui basin, a special basin, occurred after the Caledonian orogeny, in the south of Guizhou, the west of Guangxi and the southeast of Yunnan, experienced three periods: it began in the Devonian, persisted in the Carboniferous, and became fiercer in the Permian. Controlled by syndepositional fault-zones, varieties of isolated carbonate platforms, large and small, were developed in the background of a deep-water basin, namely, an inter-platform ditch. And a special paleogeographical Late Paleozoic pattern marked by"platform-basin-hill-trough" was produced in both the Dianqiangui basin and its adjacent areas. Affected by regional tectonic activities and the global changes in the sea level, the platform carbonates and coal measures superimposed each other cyclically on the attached platform. The reef-building on the isolated platform and the margin of the attached platform corresponds to the development of the shale succession in the deepwater basin. All of these elementary characteristics reflect a regular and sophisticated filling succession of the Dianqiangui basin, a result of the dual controls of the regionally tectonic activities and the eustacy. Based on the two elementary features of the third-order sequences, i.e. the regularity of sedimentary-facies succession in space and the simultaneity of environmental changes in time, 25 third-order sequences could be discerned in the Upper Paleozoic strata in the Dianqiangui basin and its adjacent areas. On the basis of the two kinds of facies-changing surfaces and the two kinds of diachronisms in stratigraphic records, the regional Late Paleozoic sequence-stratigraphic framework in the Dianqiangui basin and its adjacent areas can be established. There are two types of facies-changing surfaces and two types of diachronisms in stratigraphic records: the static type, a result of the change in sedimentary facies in space, and the dynamic type, a result of the change in time. These two types of facies-changing surfaces led to the generation of the two types of diachronisms: the diachronism of facies-changing surfaces that was formed by the static facies-changing surfaces, and the diachronism of punctuated surfaces that was formed by the dynamic facies-changing surfaces. The two types of facies-changing surfaces and the two types of diachronisms in stratigraphic records are the key to the establishment of the sequence-stratigraphic framework. The sequence boundaries could be divided geologically into fourtypes: tectonic unconformity, sedimentary unconformity, drowned unconformity and their correlative surfaces. All of these four types can be further grouped into exposed punctuated surfaces and deepened punctuated surfaces. The tectonic unconformity is similar to TypeⅠ sequence boundary, and the sedimentary unconformity is similar to TypeⅡ sequence boundary defined by Vail et al.. In terms of sequence stratigraphy, the tectonic unconformities of the Ziyun movement, the Qiangui epeirogeny and the Dongwu revolution as well as the drowned unconformity in the transitional period from the Permian to the Triassic can be systematically defined and their geological characteristics are briefly presented.

     

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  • Chen, H. M., Wu, X. H., Zhang, Y., et al., 1994. Carboniferous Lithofacies Paleogeography and Mineralization. Geological Publishing House, Beijing. 1-117 (in Chinese)
    Chen, Z. Q., 1995. The Globally Drowned Events at the End of Permian. Sedimentary Facies and Paleogeography, 15 (3): 70-76 (in Chinese)
    Comez, J. J., 1994. Condensed Processes in ShallowPlatform. Sedimentary Geology, 92: 147-159 doi: 10.1016/0037-0738(94)90103-1
    Dong, W. P., 1997. Lithostratigraphy in Guizhou. China University of Geosciences Press, Wuhan. 143-220 (in Chinese)
    Enos, P., 1995. Permian of China. In: Scholle, P. A., Peryt, T. M., Ulmer-Scholle, D. S., eds., The Permian of Northern Pangea, Vol 2. Springer, New York. 225-256
    Enos, P., Wei, J., Lehrmann, D. J., 1998. Death in Guizhou—Late Triassic Drowned of the Yangtze Carbonate Platform. Sedimentary Geology, 118: 55-76 doi: 10.1016/S0037-0738(98)00005-0
    Enos, P., Wei, J., Yan, Y., 1997. Facies Distribution and Retreat of Middle Triassic Platform Margin, Guizhou Province, South China. Sedimentology, 44: 563-584 doi: 10.1046/j.1365-3091.1997.d01-34.x
    Fan, J. S., 1990. Permian Organic—Reef. Science Press, Beijing. 1-419 (in Chinese)
    Feng, Z. Z., Jin, Z. K., Yang, Y. Q., et al., 1997. Permian Lithofacies Paleogeography in South China. Geological Publishing House, Beijing. 1-208 (in Chinese)
    Feng, Z. Z., Yang, Y. Q., Bao, Z. D., et al., 1998. Carboniferous Lithofacies Paleogeography in South China. Geological Publishing House, Beijing. 1-256 (in Chinese)
    Feng, Z. Z., Jin, Z. K., Yang, Y. Q., et al., 1994. Lithofacies Paleogeography of Permian of Yunnan-Guizhou-Guangxi Region. Geological Publishing House, Beijing. 1-129 (in Chinese)
    Goldhammer, R. K., Dunn, P. A., Hardie, L. A., 1990. Depositional Cycles, Composite Sea-Level Changes, Cycle Stacking Patterns, and the Hierarchy of Stratigraphic Forcing: Example from Alpine Triassic Platform Carbonate. Geol. Soc. Am. Bull., 102: 535-562 doi: 10.1130/0016-7606(1990)102<0535:DCCSLC>2.3.CO;2
    Hou, H. F., Cao, X. D., Wang, S. T., et al., 2000. Chinese Stratigraphic Lexicon (Devonian System). Geological Publishing House, Beijing. 3-17 (in Chinese)
    Hunt, D., Tucker, M. E., 1992. Stranded Parasequences and Forced Regressive Wedge System Tract: Deposition during BaseLevel Fall. Sedimentary Geology, 81: 1-9 doi: 10.1016/0037-0738(92)90052-S
    Jin, Y. G., Fan, Y. N., Wang, X. D., et al., 2000a. Chinese Stratigraphic Lexicon (Carboniferous System). Geological Publishing House, Beijing. 138 (in Chinese)
    Jin, Y. G., Shang, Q. H., Hou, J. P., et al., 2000b. Chinese Stratigraphic Lexicon (Permian System). Geological Publishing House, Beijing. 149 (in Chinese)
    Johson, J. G., Klapper, G., 1992. North American Midcontinent Devonian T-R Cycles. Oklahoma Geological Survey Bulletin, 145: 127-135
    Kuang, G. D., Li, J. X., Zhong, K., et al., 1999. Carboniferous of Guangxi. China University of Geosciences Press, Wuhan. 1-258 (in Chinese)
    Kuang, G. D., Zhao, M. T., Tao, Y. B., 1989. The Standard Devonian Section of China: Liujing Section of Guangxi. China University of Geosciences Press, Wuhan. 1-154 (in Chinese)
    Liu, B. J., Xu, X. S., 1994. Atlas of Sedimentary Facies and Paleogeography in South China. Science Press, Beijing. 126-144 (in Chinese)
    Liu, B. J., Xu, X. S., Pan, X. N., et al., 1993. The Sedimentary Evolution of the Crust in South China Paleocontinent andMineralization. Geological Publishing House, Beijing. 1-288 (in Chinese)
    Mei, M. X., 1995. Carbonate Cycles and Sequences. Science and Technology Press of Guizhou, Guiyang. 206 (in Chinese)
    Mei, M. X., 1996a. On the Perplexity of Lithostratigraphy According to the Natures of Stratigraphic Records. Journal of Stratigraphy, 20 (3): 207-212 (in Chinese with English Abstract)
    Mei, M. X., 1996b. Third-Order Carbonate Cyclic Sequences of Drowned Unconformity Type with Discussion on Condensation of Carbonate Platforms. Sedimentary Facies and Paleogeography, 16 (6): 24-33 (in Chinese)
    Mei, M. X., Ma, Y. S., 2001. On Two Kinds of Facies-Change Surface and Two Kinds of Diachronism in Stratigraphical Records According to the Natures of Cyclic-Sequences. Journal of Stratigraphy, 25 (2): 150-153 (in Chinese with English Abstract)
    Mei, M. X., Ma, Y. S., Dai, S. W., 2001. Late Paleozoic Filling Succession of the Dianqiangui Basin and the Division of Association of Oil-Generating Strata, Reservoir, and Capping Bed. Geoscience, 15 (1): 74-82 (in Chinese with English Abstract)
    Mitchum, R. M., 1991. High-Frequency Sequences and TheirStacking Patterns: Sequence-Stratigraphic Evidences of High-Frequency Eustatic Cycles. Sedimentary Geology, 70: 131-160 doi: 10.1016/0037-0738(91)90139-5
    Qiao, X. F., Peng, Y., Gao, L. Z., 2002. Interpretation of the Seismic Origin of Permian Limestone Dikes in Northwestern Guangxi. Geological Bulletin of China, 21 (2): 102-104 (in Chinese with English Abstract)
    Ross, C. A., Ross, J. R. P., 1995. Late Paleozoic Depositional Sequences Are Synchronism and Worldwide. Geology, 13: 194-197
    Tucker, M. E., 2001. Sedimentary Petrology. Third Edition. Blackwell Sciences, Oxford. 11-65
    Vail, P. R., Mitchum, R. M., Thompson, S., 1977. Seismic Stratigraphy and Global Changes of Sea Level, Part 3: Relative Changes of Sea Level. Am. Assoc. Petrol. Geol., Memoir, 26: 63-81
    Van Wagoner, T. C., Mitchum, R. M., Compion, K, M., et al., 1990. Siliciclastic Sequence Stratigraphy in Well Logs, Core, and Outcrops: Concepts for High-Resolution Correlation of Time and Facies. Am. Assoc. Petrol. Geol., Methods of Exploration Series, 7: 1-55
    Wang, C. S., Cheng, H. D., Shou, J. F., et al., 1999. Characteristics and Correlation of Permian Depositional Sequences in South China. Acta Sedimentologica Sinica, 17 (4): 74-82 (in Chinese with English Abstract)
    Wang, L. T., Lu, Y. B., Zhao, S. J., et al., 1994. Permian Lithofacies Paleogeography and Mineralization in South China. Geological Publishing House, Beijing. 1-137 (in Chinese)
    Wang, S. H., Fan, J. S., 1995. The Cementation of Permian Reef in Ziyun of Guizhou Province. Scientia Geologica Sinica, 30 (1): 53-62 (in Chinese with English Abstract)
    Wang, Y., Sheng, J. Z., Chen, C. X., et al., 1963. Two Sections of Permian: The Bianzhai Section in Qinglong of Pu' an County and Zisong Section of Wangmo County in Guizhou Province. In: The National Stratigraphical Committee of China, ed., The Corpus of Thesis on Chinese Stratigraphical Congress. Science Press, Beijing. 46-58 (in Chinese)
    Wu, H. R., 2000. A Discussion on the Tectonic Paleogeography Related to the CaledonianMovement inGuangxi. Journal of Paleogeography, 2 (1): 70-76 (in Chinese with English Abstract)
    Wu, Y., Du, Y. S., Gong, Y. M., 1997. Devonian Sequence Stratigraphy and the Relative Sea-Level Changes in South China. China University of Geosciences Press, Wuhan. 1-98 (in Chinese)
    Wu, Y., Zhou, H. L., Jiang, T. C., et al., 1987. The Sedimentary Facies Paleogeography and Relatively Mineral Deposits of Devonian in Guangxi. Guangxi People's Publishing House, Nanning. 1-256 (in Chinese)
    Yin, B. A., 1997. Lithostratigraphy in Guangxi. China University of Geosciences Press, Wuhan. 52-191 (in Chinese)
    Yin, H. F., Tong, J. N., Ding, M. H., 1994. Sea Level Changes from the Late Permian to the Middle Triassic in Yangtze Region. Earth Science—Journal of China University of Geosciences, 19 (5): 627-632 (in Chinese with English Abstract)
    Yin, Z. X., Zhang, S. X., Xie, C. H., 1978. A Discussion on Fold Episodes. Science Press, Beijing. 1-78 (in Chinese)
    Zeng, Y. F., Zhang, J. Q., Liu, W. J., et al., 1994. Devonian Lithofacies Paleogeography and Mineralization in South China. Geological Publishing House, Beijing. 1-119 (in Chinese)
    Zhang, W., Fan, J. S., Wu, Y. S., 1992. Permian Organic-Reef and Paleoecology. Geological Publishing House, Beijing. 1-268 (in Chinese)
    Zhang, Y. X., 2001. Diachronism of Cambrian Strata on the North China Platform. Sedimentary Geology and Tethyan Geology, 21 (1): 78-87 (in Chinese with English Abstract)
    Zhang, Y. Z., 1997. Lithostratigraphy in Yunnan. China University of Geosciences Press, Wuhan. 101-201 (in Chinese)
    Zhao, Z. Q., Ding, Q. X., 1996. The Regional Stratigraphy in Central and South Part of China. China University of Geosciences Press, Wuhan. 71-118 (in Chinese)
    Zhong, K., Wu, Y., Yin, B. A., et al., 1992. Devonian System of Guangxi. China University of Geosciences Press, Wuhan. 1-370 (in Chinese)
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