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Tong Jinnan, Li Hongli. Sequence Stratigraphy in the Littoral Carbonate Bank Zone-Lower Triassic Sequence Analysis of Songshan, Wuxi, Jiangsu[J]. Acta Sedimentologica Sinica, 1997, 15(4): 1-4.
Citation: Tong Jinnan, Li Hongli. Sequence Stratigraphy in the Littoral Carbonate Bank Zone-Lower Triassic Sequence Analysis of Songshan, Wuxi, Jiangsu[J]. Acta Sedimentologica Sinica, 1997, 15(4): 1-4.

Sequence Stratigraphy in the Littoral Carbonate Bank Zone-Lower Triassic Sequence Analysis of Songshan, Wuxi, Jiangsu

  • Received Date: 1996-08-20
  • Publish Date: 1997-12-10
  • The littoral carbonate bank section has not only the most sensitive record of the sea level change butalso the distinctive parasequence pattern.By the inimitable method of sequence recognition the carbonatebank section of Songshan, Wuxi is particular and typical in studying the Middle and Lower Yangtze re-gion stratigraphycally.The analysis of the depositional site associated with microgeography is availableand reliable method in studying the sequence and parasequence.
  • [1] (1) Yin Hongfu, Wu Shunbao, Ding Meihua, et al.The MeishanSection - - Candidate of the Global Stratotype Section andPoint (GSSP) of the Permian - Triassic Boundary (PTB).Al-beratiana, 1994, 14: 14~31.

    (2) Tong Jinnan and Yin Hongfu.Lower Triassic sequence stratig-raphy of Lower Yang tze, China.Journal of Geology, Ser.B,1995, (5- 6): 169~170.

    (3) 王恕一,朱洪发,陈亚中等.无锡嵩山长兴期海绵生物礁的发现及其意义.地层学杂志, 1990, 14(4): 308~310.

    (4) Yin Hongfu and Tong Jinnan.Relationship between sequencestratig raphical boundary and chronostratig raphical boundary.Chinese Science Bulletin.1995, 40(16): 1357~1362.

    (5) 张克信,童金南,殷鸿福等.浙江长兴二叠 - 三叠系界线剖面层序地层研究.地质学报, 1996, 70(3): 270~281.
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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  • Received:  1996-08-20
  • Published:  1997-12-10

Sequence Stratigraphy in the Littoral Carbonate Bank Zone-Lower Triassic Sequence Analysis of Songshan, Wuxi, Jiangsu

Abstract: The littoral carbonate bank section has not only the most sensitive record of the sea level change butalso the distinctive parasequence pattern.By the inimitable method of sequence recognition the carbonatebank section of Songshan, Wuxi is particular and typical in studying the Middle and Lower Yangtze re-gion stratigraphycally.The analysis of the depositional site associated with microgeography is availableand reliable method in studying the sequence and parasequence.

Tong Jinnan, Li Hongli. Sequence Stratigraphy in the Littoral Carbonate Bank Zone-Lower Triassic Sequence Analysis of Songshan, Wuxi, Jiangsu[J]. Acta Sedimentologica Sinica, 1997, 15(4): 1-4.
Citation: Tong Jinnan, Li Hongli. Sequence Stratigraphy in the Littoral Carbonate Bank Zone-Lower Triassic Sequence Analysis of Songshan, Wuxi, Jiangsu[J]. Acta Sedimentologica Sinica, 1997, 15(4): 1-4.
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